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<article xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:oasis="http://docs.oasis-open.org/ns/oasis-exchange/table" xml:lang="en" dtd-version="3.0" article-type="research-article">
  <front>
    <journal-meta><journal-id journal-id-type="publisher">AMT</journal-id><journal-title-group>
    <journal-title>Atmospheric Measurement Techniques</journal-title>
    <abbrev-journal-title abbrev-type="publisher">AMT</abbrev-journal-title><abbrev-journal-title abbrev-type="nlm-ta">Atmos. Meas. Tech.</abbrev-journal-title>
  </journal-title-group><issn pub-type="epub">1867-8548</issn><publisher>
    <publisher-name>Copernicus Publications</publisher-name>
    <publisher-loc>Göttingen, Germany</publisher-loc>
  </publisher></journal-meta>
    <article-meta>
      <article-id pub-id-type="doi">10.5194/amt-18-1243-2025</article-id><title-group><article-title>Development of a portable laser-flash photolysis Faraday rotation spectrometer for measuring atmospheric total OH reactivity</article-title><alt-title>Development of a portable laser-flash photolysis Faraday rotation spectrometer</alt-title>
      </title-group>
      <contrib-group>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Fang</surname><given-names>Bo</given-names></name>
          
        <ext-link>https://orcid.org/0000-0001-9909-1317</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Wei</surname><given-names>Nana</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="yes" rid="aff1">
          <name><surname>Zhao</surname><given-names>Weixiong</given-names></name>
          <email>wxzhao@aiofm.ac.cn</email>
        <ext-link>https://orcid.org/0000-0003-1700-8992</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Yang</surname><given-names>Nana</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Zhou</surname><given-names>Hao</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1 aff2">
          <name><surname>Zhang</surname><given-names>Heng</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Li</surname><given-names>Jiarong</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="yes" rid="aff1">
          <name><surname>Zhang</surname><given-names>Weijun</given-names></name>
          <email>wjzhang@aiofm.ac.cn</email>
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff3 aff4">
          <name><surname>Lu</surname><given-names>Yanyu</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff4 aff5">
          <name><surname>Zhu</surname><given-names>Zhu</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff4 aff5">
          <name><surname>Liu</surname><given-names>Yue</given-names></name>
          
        </contrib>
        <aff id="aff1"><label>1</label><institution>Laboratory of Atmospheric Physico-Chemistry, Anhui Institute of Optics and Fine Mechanics, HFIPS, Chinese Academy of Sciences, Hefei 230031, Anhui, China</institution>
        </aff>
        <aff id="aff2"><label>2</label><institution>Institutes of Physical Science and Information Technology, Anhui University, Hefei 230039, Anhui, China</institution>
        </aff>
        <aff id="aff3"><label>3</label><institution>Anhui Institute of Meteorological Sciences, Anhui Province Key Laboratory of Atmospheric Science and Satellite Remote Sensing, Hefei 230031, Anhui, China</institution>
        </aff>
        <aff id="aff4"><label>4</label><institution>Shouxian National Climatology Observatory, Huaihe River Basin Typical Farm Eco-meteorological Experiment Field of CMA, Shouxian 232200, Anhui, China</institution>
        </aff>
        <aff id="aff5"><label>5</label><institution>Anhui Shouxian Meteorological Bureau, Shouxian 232200, Anhui, China</institution>
        </aff>
      </contrib-group>
      <author-notes><corresp id="corr1">Weixiong Zhao (wxzhao@aiofm.ac.cn) and Weijun Zhang (wjzhang@aiofm.ac.cn)</corresp></author-notes><pub-date><day>11</day><month>March</month><year>2025</year></pub-date>
      
      <volume>18</volume>
      <issue>5</issue>
      <fpage>1243</fpage><lpage>1256</lpage>
      <history>
        <date date-type="received"><day>1</day><month>November</month><year>2024</year></date>
           <date date-type="accepted"><day>16</day><month>January</month><year>2025</year></date>
           <date date-type="rev-recd"><day>7</day><month>January</month><year>2025</year></date>
           <date date-type="rev-request"><day>11</day><month>November</month><year>2024</year></date>
      </history>
      <permissions>
        <copyright-statement>Copyright: © 2025 Bo Fang et al.</copyright-statement>
        <copyright-year>2025</copyright-year>
      <license license-type="open-access"><license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri" xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p></license></permissions><self-uri xlink:href="https://amt.copernicus.org/articles/18/1243/2025/amt-18-1243-2025.html">This article is available from https://amt.copernicus.org/articles/18/1243/2025/amt-18-1243-2025.html</self-uri><self-uri xlink:href="https://amt.copernicus.org/articles/18/1243/2025/amt-18-1243-2025.pdf">The full text article is available as a PDF file from https://amt.copernicus.org/articles/18/1243/2025/amt-18-1243-2025.pdf</self-uri>
      <abstract><title>Abstract</title>

      <p id="d2e203">Quantitative measurements of atmospheric total OH reactivity (<inline-formula><mml:math id="M1" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula>) provide crucial insights into atmospheric photochemistry. However, widespread application of total OH reactivity measurements is challenging due to insufficient equipment and the complexity of existing instrumentation. In this work, we report the development of a portable laser-flash photolysis Faraday rotation spectroscopy (LP-FRS) instrument for real-time and in situ measurement of <inline-formula><mml:math id="M2" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula>. To achieve efficient overlapping between the pump and probe laser and realize a long effective absorption path length, thus enabling high-sensitivity measurement, a specific Herriott-type pump–probe optical multi-pass cell was designed. The instrument's optical box dimensions were 130 <inline-formula><mml:math id="M3" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M4" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 40 <inline-formula><mml:math id="M5" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M6" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 35 <inline-formula><mml:math id="M7" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula>. The obtained effective absorption path was <inline-formula><mml:math id="M8" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 28.5 <inline-formula><mml:math id="M9" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi></mml:mrow></mml:math></inline-formula> in a base length of 77.2 <inline-formula><mml:math id="M10" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula>. The <inline-formula><mml:math id="M11" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> detection precisions of the LP-FRS instrument were 2.3 and 1.0 <inline-formula><mml:math id="M12" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> with averaging times of 60 and 300 <inline-formula><mml:math id="M13" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">s</mml:mi></mml:mrow></mml:math></inline-formula>, respectively. The <inline-formula><mml:math id="M14" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> measurement uncertainty was evaluated to be within 2 <inline-formula><mml:math id="M15" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>. Field measurement was performed, and the difference between the measured <inline-formula><mml:math id="M16" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> and the model simulated from the measured reactive species was analysed. The developed portable LP-FRS instrument extends the measurement methods of atmospheric total OH reactivity and has certain advantages in terms of cost, operation, and transportation, which will play an increasingly important role in future atmospheric chemistry research.</p>
  </abstract>
    
<funding-group>
<award-group id="gs1">
<funding-source>National Key Research and Development Program of China</funding-source>
<award-id>2022YFC370030401</award-id>
<award-id>2023YFC3705502</award-id>
</award-group>
<award-group id="gs2">
<funding-source>National Natural Science Foundation of China</funding-source>
<award-id>U21A2028</award-id>
<award-id>42105099</award-id>
<award-id>91544228</award-id>
</award-group>
</funding-group>
</article-meta>
  </front>
<body>
      

<sec id="Ch1.S1" sec-type="intro">
  <label>1</label><title>Introduction</title>
      <p id="d2e384">The hydroxyl (OH) radical is the most important oxidant in the atmosphere during daytime. It initiates the oxidation of most natural and anthropogenic trace gas species, thereby dominating their atmospheric lifetimes. Knowledge of tropospheric OH chemistry contributes to our understanding of air pollution and climate change (Lu et al., 2018; Nicely et al., 2018). However, due to the large number (10<sup>4</sup>–10<sup>5</sup>) of volatile organic compounds (VOCs) (Goldstein and Galbally, 2007), a comprehensive interpretation of the sink mechanisms of OH is extremely challenging.</p>
      <p id="d2e405">Total OH reactivity (<inline-formula><mml:math id="M19" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula>), the inverse of the OH chemical lifetime (<inline-formula><mml:math id="M20" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula>), serves as a crucial parameter for estimating the total loss rate of OH due to all atmospheric OH reactants (Yang et al., 2016). It is defined as the sum of OH reactant concentrations (<inline-formula><mml:math id="M21" display="inline"><mml:mrow><mml:mo>[</mml:mo><mml:mi>X</mml:mi><mml:mo>]</mml:mo></mml:mrow></mml:math></inline-formula>) weighted by their reaction rate coefficient with OH (<inline-formula><mml:math id="M22" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mrow><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>+</mml:mo><mml:mi>X</mml:mi></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula>), which can be expressed as
          <disp-formula id="Ch1.E1" content-type="numbered"><label>1</label><mml:math id="M23" display="block"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup><mml:mo>=</mml:mo><mml:msubsup><mml:mi mathvariant="italic">τ</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msubsup><mml:mo>=</mml:mo><mml:mo movablelimits="false">∑</mml:mo><mml:msub><mml:mi>k</mml:mi><mml:mrow><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>+</mml:mo><mml:msub><mml:mi>X</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:msub><mml:mo>[</mml:mo><mml:msub><mml:mi>X</mml:mi><mml:mi>i</mml:mi></mml:msub><mml:mo>]</mml:mo><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
        where <inline-formula><mml:math id="M24" display="inline"><mml:mrow><mml:msub><mml:mi>X</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> is the <inline-formula><mml:math id="M25" display="inline"><mml:mi>i</mml:mi></mml:math></inline-formula>th reactant. Measurement of <inline-formula><mml:math id="M26" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> provides a powerful tool for both field campaigns and laboratory studies in atmospheric photochemistry (Stone et al., 2012; Fuchs et al., 2013). The balance between OH production and loss rate provides additional information on the OH sources (Martinez et al., 2003; Hens et al., 2014). The difference between measured and calculated <inline-formula><mml:math id="M27" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> can be used to estimate the contribution from individually measured species, the total missing reactivity, and the role of unknown VOCs (Di Carlo et al., 2004; Mao et al., 2010; Sinha et al., 2012). The measured total OH reactivity can also be used as the chemical closure of the reactive carbon budget (Hunter et al., 2017; Safieddine et al., 2017; Heald et al., 2020). In addition, <inline-formula><mml:math id="M28" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> measurements help to estimate instantaneous production potential and the production regime of ozone (Sinha et al., 2012; Li et al., 2021, 2022; Kohno et al., 2022). Recently, the long-term trend in <inline-formula><mml:math id="M29" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> has been proven to be a key atmospheric oxidation capacity parameter for the formulation of ozone (<inline-formula><mml:math id="M30" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>) pollution mitigation strategies (Wang et al., 2023).</p>
      <p id="d2e606">Several methods for OH reactivity measurement have been developed (Yang et al., 2016; Fuchs et al., 2017), which can be divided into three categories: the indirect method, known as the comparative reactivity method (CRM) (Sinha et al., 2008, Kumar and Sinha, 2014; Michoud et al., 2015; Kim et al., 2016; Praplan et al., 2017; Yang et al., 2017); the semi-direct technique, involving flow tube–chemical ionization mass spectrometry (FT-CIMS) (Muller et al., 2018); and the direct method, including flow tube–laser-induced fluorescence (FT-LIF) (Kovacs and Brune, 2001; Mao et al., 2009; Ingham et.al., 2009; Hansen et al., 2014) and laser-flash photolysis–laser-induced fluorescence (LP-LIF) (Sadanaga et al., 2004; Lou et al., 2010; Parker et al., 2011; Stone et al., 2016).</p>
      <p id="d2e609">The CRM indirectly determines <inline-formula><mml:math id="M31" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> by the competitive kinetics for OH between a reference molecule not present in normal atmospheric conditions (e.g. pyrrole) and all reactive atmospheric species in ambient air. Commercial proton-transfer-reaction mass spectrometry (PTR-MS) or gas chromatography (GC) is employed to detect the concentration change in pyrrole (Nölscher et al., 2012). The direct method determined <inline-formula><mml:math id="M32" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> from the measured time-dependent OH decay. The FT-LIF directly measures OH decay by controlling the reaction time through the movement of an OH injector along a flow tube. An LIF instrument is positioned downstream of the flow tube to monitor the OH concentration signal intensity. The sample is then drawn into the low-pressure (<inline-formula><mml:math id="M33" display="inline"><mml:mo lspace="0mm">∼</mml:mo></mml:math></inline-formula> 1.5 <inline-formula><mml:math id="M34" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">Torr</mml:mi></mml:mrow></mml:math></inline-formula>) cell of the LIF via gas expansion. A 308 <inline-formula><mml:math id="M35" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">nm</mml:mi></mml:mrow></mml:math></inline-formula> dye laser is used to excite OH, and the resulting 308 <inline-formula><mml:math id="M36" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">nm</mml:mi></mml:mrow></mml:math></inline-formula> fluorescence emitted by OH is collected for concentration evaluation. The LP-LIF is a pump–probe technique where OH decay can be observed with high time resolution after each flash, without needing to determine the reaction time from the point of OH production to the sampling position. In this technique, OH is produced by laser-flash photolysis of <inline-formula><mml:math id="M37" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> at 266 <inline-formula><mml:math id="M38" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">nm</mml:mi></mml:mrow></mml:math></inline-formula> across the entire illuminated area in the presence of water vapour. This makes it less susceptible to the recycling process caused by nitric oxide (NO) compared to the above instruments using water vapour photolysis (Sadanaga et al., 2004; Lou et al., 2010) because water vapour photolysis with a 184.9 <inline-formula><mml:math id="M39" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">nm</mml:mi></mml:mrow></mml:math></inline-formula> ultraviolet (UV)  lamp not only generates OH but also produces <inline-formula><mml:math id="M40" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">HO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> radicals. In the presence of high atmospheric NO concentrations, the reaction of <inline-formula><mml:math id="M41" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">HO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> with NO can lead to the reformation of OH, which may affect the measurement of <inline-formula><mml:math id="M42" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula>. In the semi-direct technique of FT-CIMS, sulfuric acid (<inline-formula><mml:math id="M43" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>) instead of OH is measured by a CIMS instrument to record the data point of OH decay at each reaction time. The reaction time can be varied by adding 10 ppmv <inline-formula><mml:math id="M44" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> at different fixed positions within the flow tube. Due to the titration reaction, OH is nearly completely converted to <inline-formula><mml:math id="M45" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, so the measured change in the <inline-formula><mml:math id="M46" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> concentration serves as an indicator of the OH.</p>
      <p id="d2e796">Several intercomparisons of the techniques and instruments mentioned above have been conducted. Zannoni et al. (2015) reported a field intercomparison of two CRM instruments in the Mediterranean Basin. Hansen et al. (2015) carried out an intercomparison between the CRM and LP-LIF techniques in an urban environment. The series of intercomparison experiments conducted in the SAPHIR simulation chamber at Forschungszentrum Jülich involved all types of existing methods and nine instruments from around the world (Fuchs et al., 2017). The results show that indirect or semi-direct methods exhibit more scatter in measurements and are most likely limited by the corrections for known effects, such as high NO concentrations for CRM and high-reactivity conditions for FT-CIMS. In comparison, the direct methods (LIF) that combine laser-flash photolysis offer advantages in detection precision and accuracy. Overall, the existing techniques can give reasonable measurement results for a wide range of atmospheric conditions. However, the high cost of development and operation (e.g. the expensive and complex dye laser system and mass spectrometer system), limited instruments, the complex operation and calibration procedures, and the relatively large size of these instruments hinder the widespread application of measuring OH reactivity.</p>

      <fig id="Ch1.F1" specific-use="star"><label>Figure 1</label><caption><p id="d2e801"><bold>(a)</bold> Schematic diagram of the developed laser-flash photolysis Faraday rotation spectrometer (LP-FRS), which consists of a mid-infrared Faraday rotation spectroscopy system and a laser photolysis system. The OH radicals are generated by laser-flash photolysis at 266 <inline-formula><mml:math id="M47" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">nm</mml:mi></mml:mrow></mml:math></inline-formula> in a Herriott cell wound with copper wires and detected simultaneously by Faraday rotation spectroscopy via the overlapping mid-infrared optical paths. P, polarizer; FM, foldable mirror; SM, silver mirror; L, lens; PD, photodetector; YM, <inline-formula><mml:math id="M48" display="inline"><mml:mrow class="chem"><mml:mi mathvariant="normal">Nd</mml:mi><mml:mo>:</mml:mo><mml:mi mathvariant="normal">YAG</mml:mi></mml:mrow></mml:math></inline-formula> mirror; BE, beam expander; DAQ, data acquisition card. <bold>(b)</bold> Assembly diagram of the Herriott-type pump–probe multi-pass cell (MPC). The coil is wound around the body of the MPC. A water-cooling interlayer is designed for temperature control of the solenoid coil and the cell.</p></caption>
        <graphic xlink:href="https://amt.copernicus.org/articles/18/1243/2025/amt-18-1243-2025-f01.png"/>

      </fig>

      <p id="d2e835">In this work, we report the development of a portable laser-flash photolysis Faraday rotation spectroscopy (LP-FRS) instrument for total OH reactivity measurement. The time-resolved LP-FRS is a novel technique that employs a mid-infrared semiconductor diode laser as the probe laser (with a much cheaper commercial price than the dye laser system and good stability) for <inline-formula><mml:math id="M49" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> measurement, making the technique both cost-effective and simple to operate (Wei et al., 2020). Since FRS relies on the detection of the probe light polarization state rotation induced by paramagnetic molecules in a longitudinal magnetic field, the laser noise and molecule interferences are significantly reduced, which enables the FRS system to directly and completely monitor the concentration of OH in a highly sensitive manner without any chemical interferences (Litfin et al., 1980; Zhao et al., 2018). The dimensions of the developed instrument were 130 <inline-formula><mml:math id="M50" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M51" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 40 <inline-formula><mml:math id="M52" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M53" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 35 <inline-formula><mml:math id="M54" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula>. The achievable detection precision of <inline-formula><mml:math id="M55" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> was 1.0 <inline-formula><mml:math id="M56" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> with 300 <inline-formula><mml:math id="M57" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">s</mml:mi></mml:mrow></mml:math></inline-formula> averaging time. A field test in a suburban area was performed to demonstrate the capability of the LP-FRS instrument.</p>
</sec>
<sec id="Ch1.S2">
  <label>2</label><title>Experimental setup</title>
      <p id="d2e935">A schematic diagram of the developed LP-FRS instrument is given in Fig. <xref ref-type="fig" rid="Ch1.F1"/>a. The instrument comprises a mid-infrared FRS system for direct measurement of OH and an ultraviolet (UV) laser-flash photolysis system for generating OH. The probe light and the UV beam overlap in a Herriott-type optical multi-pass cell (MPC), enabling simultaneous monitoring of OH by the FRS system during the generation and reaction with reactants. Optical components from both systems are integrated into a single unitary box, with all communications and gas tubes connected to designated interfaces. The optical box has dimensions of 130 <inline-formula><mml:math id="M58" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M59" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 40 <inline-formula><mml:math id="M60" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M61" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 35 <inline-formula><mml:math id="M62" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> and a total weight of <inline-formula><mml:math id="M63" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 90 <inline-formula><mml:math id="M64" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">kg</mml:mi></mml:mrow></mml:math></inline-formula>. The instrument's total operation power consumption is <inline-formula><mml:math id="M65" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 3 <inline-formula><mml:math id="M66" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">kW</mml:mi></mml:mrow></mml:math></inline-formula>. These factors make the developed LP-FRS instrument both cost-effective and portable for field applications.</p>
<sec id="Ch1.S2.SS1">
  <label>2.1</label><title>Mid-infrared Faraday rotation spectrometer</title>
      <p id="d2e1016">A mid-infrared continuous-wave distributed-feedback laser (cw-DFB laser, Nanoplus GmbH) emitting at 2.8 <inline-formula><mml:math id="M67" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi><mml:mi mathvariant="normal">m</mml:mi></mml:mrow></mml:math></inline-formula> is used as the probe laser. The current and temperature of the laser chip are controlled by a laser controller (LDC501, Stanford Research Systems). By changing the injection current from 90 to 130 <inline-formula><mml:math id="M68" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">mA</mml:mi></mml:mrow></mml:math></inline-formula> at an operating temperature of 33 <inline-formula><mml:math id="M69" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">°</mml:mi><mml:mi mathvariant="normal">C</mml:mi></mml:mrow></mml:math></inline-formula>, the wavelength of the DFB laser can be tuned from 3568.939 to 3568.362 <inline-formula><mml:math id="M70" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>. The current tuning coefficient is about 0.0024 <inline-formula><mml:math id="M71" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">mA</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> near the target Q(1.5e) line of the <inline-formula><mml:math id="M72" display="inline"><mml:mrow><mml:msup><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:msub><mml:mi mathvariant="normal">Π</mml:mi><mml:mrow><mml:mn mathvariant="normal">3</mml:mn><mml:mo>/</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula> state of OH at 3568.523 <inline-formula><mml:math id="M73" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>. The selected line has the strongest line strength of <inline-formula><mml:math id="M74" display="inline"><mml:mi>S</mml:mi></mml:math></inline-formula> <inline-formula><mml:math id="M75" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 9.032 <inline-formula><mml:math id="M76" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<sup>−20</sup> <inline-formula><mml:math id="M78" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mo>(</mml:mo><mml:mi mathvariant="normal">molec</mml:mi><mml:mo>.</mml:mo><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula> at 296 <inline-formula><mml:math id="M79" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">K</mml:mi></mml:mrow></mml:math></inline-formula> (Gordon, et al., 2022) with the largest effective g<sub><italic>J</italic></sub> value of 0.936 in the infrared region, which make it preferable for the FRS detection (Zhao et al., 2011, 2012). The collimated beam output from the laser head passes through a Rochon prism (Foctek Photonics), with an extinction ratio of <inline-formula><mml:math id="M81" display="inline"><mml:mi mathvariant="italic">ξ</mml:mi></mml:math></inline-formula> <inline-formula><mml:math id="M82" display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 5 <inline-formula><mml:math id="M83" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<sup>−6</sup>, to establish a linearly polarized state, and then is incident into a Herriott-type pump–probe MPC. A <inline-formula><mml:math id="M85" display="inline"><mml:mrow class="chem"><mml:mi mathvariant="normal">He</mml:mi><mml:mo>-</mml:mo><mml:mi mathvariant="normal">Ne</mml:mi></mml:mrow></mml:math></inline-formula> laser serves as an indicator. The beam waists of both lasers are aligned at the centre of the MPC to minimize beam divergence after each reflection (Pilgrim et al., 1997). A flipper optical mount facilitates switching between the two lasers. A second Rochon prism is placed at the output path to analyse the polarization state. The exit beam from the MPC is focused on a thermoelectrically cooled mercury cadmium telluride (MCT) photodetector (PVI-4TE-3.4, VIGO system). To effectively modulate the magnetic circular birefringence in a static magnetic field (Zhao et al., 2018; Fang et al., 2020; Wei et al., 2020), a 33 <inline-formula><mml:math id="M86" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">kHz</mml:mi></mml:mrow></mml:math></inline-formula> sinusoidal wave from a lock-in amplifier (SR830, Stanford Research Systems) is added to the laser injection current. The detector signal is processed by the lock-in amplifier to demodulate the second harmonic (2<inline-formula><mml:math id="M87" display="inline"><mml:mi>f</mml:mi></mml:math></inline-formula>) of the FRS signal. As the laser current is fixed at the absorption peak of the OH radical, a time-resolved Faraday rotation spectrum that directly reflects the concentration variation in OH radicals can be measured (Wei et al., 2020; Cheng et al., 2023).</p>
      <p id="d2e1263">The pump–probe MPC, as shown in Fig. <xref ref-type="fig" rid="Ch1.F1"/>b, consists of a cylindrical stainless steel tube with an inner diameter of 5 <inline-formula><mml:math id="M88" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula>, a total length of approximately 89 <inline-formula><mml:math id="M89" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula>, and a sample volume of 1.5 <inline-formula><mml:math id="M90" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">L</mml:mi></mml:mrow></mml:math></inline-formula>. At both ends, a pair of 6.8 <inline-formula><mml:math id="M91" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> diameter calcium fluoride (<inline-formula><mml:math id="M92" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">CaF</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>) windows are used for sealing and light transmission. Two gold-coated concave spherical mirrors, each 5 <inline-formula><mml:math id="M93" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> in diameter, are spaced 77.2 <inline-formula><mml:math id="M94" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> apart within the cell. Each mirror features a 5 <inline-formula><mml:math id="M95" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">mm</mml:mi></mml:mrow></mml:math></inline-formula> diameter hole for probe light incidence and exit and a central 32 <inline-formula><mml:math id="M96" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">mm</mml:mi></mml:mrow></mml:math></inline-formula> diameter hole (i.e. the maximum diameter permissible for the UV beam passage) for the expanded photolysis beam. Mirror tilt and spacing are adjustable via three screws distributed circularly on the mirror mount. At each end of the MPC, there are eight circular quartz observation windows near the mirrors to facilitate multi-pass light adjustments. A total of 25 reflection spots are arranged on the mirror surfaces in a circular pattern with 2 <inline-formula><mml:math id="M97" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> radius. The total path length of the MPC is 37.8 <inline-formula><mml:math id="M98" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi></mml:mrow></mml:math></inline-formula>.</p>
      <p id="d2e1361">A solenoid coil, wrapped with 1 <inline-formula><mml:math id="M99" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">mm</mml:mi></mml:mrow></mml:math></inline-formula> diameter red-copper enamelled wires, is wound around the stainless steel tube and operates in DC mode to offer a static magnetic field for FRS. The length and the outer diameter of the coil are 59 <inline-formula><mml:math id="M100" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> and 10 <inline-formula><mml:math id="M101" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula>, respectively. The magnetic intensity tuning coefficient at the centre of the coil is 73 G/A. A water-cooling interlayer is designed for temperature control of both the solenoid coil and the cell.</p>
</sec>
<sec id="Ch1.S2.SS2">
  <label>2.2</label><title>Ultraviolet laser-flash photolysis system</title>
      <p id="d2e1396">A flashlamp pumped <inline-formula><mml:math id="M102" display="inline"><mml:mrow class="chem"><mml:mi mathvariant="normal">Nd</mml:mi><mml:mo>:</mml:mo><mml:mi mathvariant="normal">YAG</mml:mi></mml:mrow></mml:math></inline-formula> laser (Big Sky Laser Ultra 100, Quantel) is employed as the photolysis laser. The laser wavelength is frequency doubled to generate the fourth harmonic radiation at 266 <inline-formula><mml:math id="M103" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">nm</mml:mi></mml:mrow></mml:math></inline-formula> with a pulse energy of 25 <inline-formula><mml:math id="M104" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">mJ</mml:mi></mml:mrow></mml:math></inline-formula>, energy stability of <inline-formula><mml:math id="M105" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 2 %, pulse length of <inline-formula><mml:math id="M106" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 6 <inline-formula><mml:math id="M107" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">ns</mml:mi></mml:mrow></mml:math></inline-formula>, and beam diameter of <inline-formula><mml:math id="M108" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 4 <inline-formula><mml:math id="M109" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">mm</mml:mi></mml:mrow></mml:math></inline-formula>. The water-cooled laser head has a size of <inline-formula><mml:math id="M110" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 30.6 <inline-formula><mml:math id="M111" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M112" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 7.6 <inline-formula><mml:math id="M113" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M114" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 5.6 <inline-formula><mml:math id="M115" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> and is controlled by an integrated cooling and electronics unit. The 266 <inline-formula><mml:math id="M116" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">nm</mml:mi></mml:mrow></mml:math></inline-formula> pulse emitted from the laser head is directed coaxially into the MPC using two dielectrically coated 1 <inline-formula><mml:math id="M117" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">in</mml:mi><mml:mo>.</mml:mo></mml:mrow></mml:math></inline-formula> diameter mirrors. Prior to entering the cell, the diameter of the 266 <inline-formula><mml:math id="M118" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">nm</mml:mi></mml:mrow></mml:math></inline-formula> beam is expanded to 32 <inline-formula><mml:math id="M119" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">mm</mml:mi></mml:mrow></mml:math></inline-formula> using a beam expander consisting of a quartz concave lens with a focal length of 12.5 <inline-formula><mml:math id="M120" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">mm</mml:mi></mml:mrow></mml:math></inline-formula> and a quartz convex lens with a focal length of 100 <inline-formula><mml:math id="M121" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">mm</mml:mi></mml:mrow></mml:math></inline-formula>.</p>
      <p id="d2e1562">A digital delay generator (DG645, Stanford Research Systems) was used to control the time sequence of laser-flash photolysis to record the time-resolved OH decay curve. The pump and Q switch of the <inline-formula><mml:math id="M122" display="inline"><mml:mrow class="chem"><mml:mi mathvariant="normal">Nd</mml:mi><mml:mo>:</mml:mo><mml:mi mathvariant="normal">YAG</mml:mi></mml:mrow></mml:math></inline-formula> laser are synchronized with two 4 <inline-formula><mml:math id="M123" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">Hz</mml:mi></mml:mrow></mml:math></inline-formula> transistor–transistor logic (TTL) pulses delayed by 30 <inline-formula><mml:math id="M124" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">ms</mml:mi></mml:mrow></mml:math></inline-formula> relative to the data acquisition to achieve the baseline of the OH decay curve. The rising edges of the pulses are used for triggering. The spectrum is sampled with 1000 data points, each separated by a time interval of 0.2 <inline-formula><mml:math id="M125" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">ms</mml:mi></mml:mrow></mml:math></inline-formula>.</p>

      <fig id="Ch1.F2" specific-use="star"><label>Figure 2</label><caption><p id="d2e1603"><bold>(a)</bold> Schematic of the Herriott multi-pass cell and the beam pattern on mirror surface for the pump–probe; <bold>(b)</bold> multi-pass light waist (<inline-formula><mml:math id="M126" display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mi mathvariant="normal">c</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>), <inline-formula><mml:math id="M127" display="inline"><mml:mi>g</mml:mi></mml:math></inline-formula> value, and overlapping factor (<inline-formula><mml:math id="M128" display="inline"><mml:mi mathvariant="italic">η</mml:mi></mml:math></inline-formula>) as functions of <inline-formula><mml:math id="M129" display="inline"><mml:mi mathvariant="italic">θ</mml:mi></mml:math></inline-formula>. <inline-formula><mml:math id="M130" display="inline"><mml:mi mathvariant="italic">θ</mml:mi></mml:math></inline-formula> is half of the angle between two adjacent reflection spots. The <inline-formula><mml:math id="M131" display="inline"><mml:mi mathvariant="italic">θ</mml:mi></mml:math></inline-formula> of 158.4° is selected, achieving an <inline-formula><mml:math id="M132" display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mi mathvariant="normal">c</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M133" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 3.7 <inline-formula><mml:math id="M134" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">mm</mml:mi></mml:mrow></mml:math></inline-formula> and an <inline-formula><mml:math id="M135" display="inline"><mml:mi mathvariant="italic">η</mml:mi></mml:math></inline-formula> of 75.4 %.</p></caption>
          <graphic xlink:href="https://amt.copernicus.org/articles/18/1243/2025/amt-18-1243-2025-f02.png"/>

        </fig>

<table-wrap id="Ch1.T1" specific-use="star"><label>Table 1</label><caption><p id="d2e1701">Overlapping factor comparison of MPCs used for laser photolysis in pump–probe techniques.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="5">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="right"/>
     <oasis:colspec colnum="3" colname="col3" align="right"/>
     <oasis:colspec colnum="4" colname="col4" align="right"/>
     <oasis:colspec colnum="5" colname="col5" align="left"/>
     <oasis:thead>
       <oasis:row>
         <oasis:entry colname="col1">MPC type</oasis:entry>
         <oasis:entry colname="col2">Base length</oasis:entry>
         <oasis:entry colname="col3">Effective overlapping</oasis:entry>
         <oasis:entry colname="col4">Overlapping factor</oasis:entry>
         <oasis:entry colname="col5">References</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2">(<inline-formula><mml:math id="M136" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col3">path length (<inline-formula><mml:math id="M137" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi></mml:mrow></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col4">(%)</oasis:entry>
         <oasis:entry colname="col5"/>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>
         <oasis:entry colname="col1">Multi-pass</oasis:entry>
         <oasis:entry colname="col2">150</oasis:entry>
         <oasis:entry colname="col3">4.4</oasis:entry>
         <oasis:entry colname="col4">35.9</oasis:entry>
         <oasis:entry colname="col5">Lewis et al. (2018)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">arrangement</oasis:entry>
         <oasis:entry colname="col2">150</oasis:entry>
         <oasis:entry colname="col3">7.0</oasis:entry>
         <oasis:entry colname="col4">41.9</oasis:entry>
         <oasis:entry colname="col5">Lewis et al. (2018)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">Herriott cell</oasis:entry>
         <oasis:entry colname="col2">90</oasis:entry>
         <oasis:entry colname="col3">12</oasis:entry>
         <oasis:entry colname="col4">33.3</oasis:entry>
         <oasis:entry colname="col5">Pilgrim et al. (1997)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2">125</oasis:entry>
         <oasis:entry colname="col3">45</oasis:entry>
         <oasis:entry colname="col4">64.0</oasis:entry>
         <oasis:entry colname="col5">Pilgrim et al. (1997)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2">100</oasis:entry>
         <oasis:entry colname="col3">3.5</oasis:entry>
         <oasis:entry colname="col4">18.4</oasis:entry>
         <oasis:entry colname="col5">Qian et al. (2000)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2">73</oasis:entry>
         <oasis:entry colname="col3">13</oasis:entry>
         <oasis:entry colname="col4">80.2</oasis:entry>
         <oasis:entry colname="col5">Luo et al. (2019)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2">65.5</oasis:entry>
         <oasis:entry colname="col3">24.5</oasis:entry>
         <oasis:entry colname="col4">58.6</oasis:entry>
         <oasis:entry colname="col5">Luo and Horng (2020)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2">65.5</oasis:entry>
         <oasis:entry colname="col3">20.9</oasis:entry>
         <oasis:entry colname="col4">50</oasis:entry>
         <oasis:entry colname="col5">Luo  (2020)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2">122</oasis:entry>
         <oasis:entry colname="col3">25</oasis:entry>
         <oasis:entry colname="col4">41.7</oasis:entry>
         <oasis:entry colname="col5">Wei et al. (2020),</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2"/>
         <oasis:entry colname="col3"/>
         <oasis:entry colname="col4"/>
         <oasis:entry colname="col5">Cheng et al. (2023)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2">91.3</oasis:entry>
         <oasis:entry colname="col3">6.3</oasis:entry>
         <oasis:entry colname="col4">32.9</oasis:entry>
         <oasis:entry colname="col5">Yan et al. (2020),</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2"/>
         <oasis:entry colname="col3"/>
         <oasis:entry colname="col4"/>
         <oasis:entry colname="col5">Teng et al. (2021)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2">77.2</oasis:entry>
         <oasis:entry colname="col3">28.5</oasis:entry>
         <oasis:entry colname="col4">75.4</oasis:entry>
         <oasis:entry colname="col5">This work</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table></table-wrap>

</sec>
</sec>
<sec id="Ch1.S3">
  <label>3</label><title>Instrument performance</title>
<sec id="Ch1.S3.SS1">
  <label>3.1</label><title>Characterization of the pump–probe MPC</title>
      <p id="d2e2012">The MPC in the instrument determines the effective absorption path length of the FRS system for OH measurement (Wei et al., 2020; Yan et al., 2020). As shown in Fig. <xref ref-type="fig" rid="Ch1.F2"/>a, the mid-infrared light undergoing multiple passes between two mirrors within the MPC is used for OH detection; the expanded 266 <inline-formula><mml:math id="M138" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">nm</mml:mi></mml:mrow></mml:math></inline-formula> UV pulse is employed for producing OH. The overlapping factor (<inline-formula><mml:math id="M139" display="inline"><mml:mrow><mml:mi mathvariant="italic">η</mml:mi><mml:mo>=</mml:mo><mml:mi>l</mml:mi><mml:mo>/</mml:mo><mml:mi>d</mml:mi></mml:mrow></mml:math></inline-formula>) can be defined as the ratio of the overlapping length (<inline-formula><mml:math id="M140" display="inline"><mml:mi>l</mml:mi></mml:math></inline-formula>) to the base length (<inline-formula><mml:math id="M141" display="inline"><mml:mi>d</mml:mi></mml:math></inline-formula>) of the MPC. To develop portable instruments, increasing the overlapping factor is crucial for achieving a long effective path length while reducing the MPC base length. The Herriott MPC in the developed LP-FRS instrument is specially designed with a small multi-pass light distribution circle radius at the centre to achieve a high overlapping factor. The radius of the multi-pass light distribution circle at the centre of the Herriott MPC can be calculated with (Trutna and Byer, 1980)
            <disp-formula id="Ch1.E2" content-type="numbered"><label>2</label><mml:math id="M142" display="block"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mi mathvariant="normal">c</mml:mi></mml:msub><mml:mo>=</mml:mo><mml:mi>r</mml:mi><mml:msup><mml:mfenced close=")" open="("><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi>g</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:mo>+</mml:mo><mml:mn mathvariant="normal">2</mml:mn><mml:msub><mml:mi>g</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:msub><mml:mi>g</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mo>+</mml:mo><mml:msub><mml:mi>g</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow><mml:mrow><mml:mn mathvariant="normal">4</mml:mn><mml:msub><mml:mi>g</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:mfrac></mml:mstyle></mml:mfenced><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mo>/</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where <inline-formula><mml:math id="M143" display="inline"><mml:mi>g</mml:mi></mml:math></inline-formula> (<inline-formula><mml:math id="M144" display="inline"><mml:mrow><mml:mi>g</mml:mi><mml:mo>=</mml:mo><mml:msub><mml:mi>g</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:mo>=</mml:mo><mml:msub><mml:mi>g</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mo>=</mml:mo><mml:mi>cos⁡</mml:mi><mml:mi mathvariant="italic">θ</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">1</mml:mn><mml:mo>-</mml:mo><mml:mi>d</mml:mi><mml:mo>/</mml:mo><mml:mi>R</mml:mi></mml:mrow></mml:math></inline-formula>) is the parameter that describes the optical resonance stability of the optical cavity or MPC. When the <inline-formula><mml:math id="M145" display="inline"><mml:mi>g</mml:mi></mml:math></inline-formula> value is less than zero, the base length of the multi-pass cell exceeds the curvature radius of the mirror, causing the resonance to become unstable. An incident parallel beam or a beam whose waist is not properly aligned with the cell's centre will quickly diverge and cannot be collected. However, a beam with its waist well matched to the centre can effectively prevent divergence. <inline-formula><mml:math id="M146" display="inline"><mml:mi mathvariant="italic">θ</mml:mi></mml:math></inline-formula> is half of the angle between two adjacent reflection light points on the mirror surface. <inline-formula><mml:math id="M147" display="inline"><mml:mi>d</mml:mi></mml:math></inline-formula> is the base length, and <inline-formula><mml:math id="M148" display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:mo>=</mml:mo><mml:msub><mml:mi>R</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mo>=</mml:mo><mml:mi>R</mml:mi></mml:mrow></mml:math></inline-formula> is the curvature radii of the mirrors. <inline-formula><mml:math id="M149" display="inline"><mml:mi>r</mml:mi></mml:math></inline-formula> is the radius of the spot distribution circle.</p>
      <p id="d2e2218">Figure <xref ref-type="fig" rid="Ch1.F2"/>b illustrates the variations in <inline-formula><mml:math id="M150" display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mi mathvariant="normal">c</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M151" display="inline"><mml:mi>g</mml:mi></mml:math></inline-formula>, and <inline-formula><mml:math id="M152" display="inline"><mml:mi mathvariant="italic">η</mml:mi></mml:math></inline-formula> as functions of <inline-formula><mml:math id="M153" display="inline"><mml:mi mathvariant="italic">θ</mml:mi></mml:math></inline-formula>. When the <inline-formula><mml:math id="M154" display="inline"><mml:mi mathvariant="italic">θ</mml:mi></mml:math></inline-formula> value is below 79.2, <inline-formula><mml:math id="M155" display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mi mathvariant="normal">c</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> exceeds the 16 <inline-formula><mml:math id="M156" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">mm</mml:mi></mml:mrow></mml:math></inline-formula> radius of the photolysis beam, resulting in no overlapping path. As <inline-formula><mml:math id="M157" display="inline"><mml:mi mathvariant="italic">θ</mml:mi></mml:math></inline-formula> approaches <inline-formula><mml:math id="M158" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>1, the value of <inline-formula><mml:math id="M159" display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mi mathvariant="normal">c</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> decreases, and the <inline-formula><mml:math id="M160" display="inline"><mml:mi mathvariant="italic">η</mml:mi></mml:math></inline-formula> value increases. Considering the difficulties in processing and testing mirror curvature, <inline-formula><mml:math id="M161" display="inline"><mml:mi mathvariant="italic">θ</mml:mi></mml:math></inline-formula> was set to 158.4°, yielding an <inline-formula><mml:math id="M162" display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mi mathvariant="normal">c</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> value of 3.7 <inline-formula><mml:math id="M163" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">mm</mml:mi></mml:mrow></mml:math></inline-formula>. The achieved <inline-formula><mml:math id="M164" display="inline"><mml:mi mathvariant="italic">η</mml:mi></mml:math></inline-formula> was up to <inline-formula><mml:math id="M165" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 75.4 %, corresponding to an overlapping path length of <inline-formula><mml:math id="M166" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 28.5 <inline-formula><mml:math id="M167" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi></mml:mrow></mml:math></inline-formula>.</p>
      <p id="d2e2371">In fact, from an optical structure perspective, the overlap factor characterizes both the utilization efficiency of the optical path length and the compactness of the pump–probe MPC, making it an ideal parameter for performance characterization. To demonstrate the efforts in reducing instrument size, a comparison of effective overlapping path lengths and overlapping factors with the literature-reported pump–probe MPCs is shown in Table <xref ref-type="table" rid="Ch1.T1"/>. The effective overlapping path length of these MPCs ranged from several metres to tens of metres with base lengths around 100 <inline-formula><mml:math id="M168" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> (Pilgrim et al., 1997; Luo et al., 2019; Qian et al., 2000; Lewis et al., 2018; Luo and Horng, 2020; Luo, 2020; Wei et al., 2020; Yan et al., 2020; Teng et al., 2021; Cheng et al., 2023). The overlapping factor of our MPC was comparable to that developed by Luo et al. (2019) for a similar base length, while our effective overlapping path length was twice as long.</p>

      <fig id="Ch1.F3"><label>Figure 3</label><caption><p id="d2e2387"><bold>(a)</bold> Noise and <bold>(b)</bold> signal-to-noise ratio analysis of the FRS system. The optimum offset angle of the analyser is 8°.</p></caption>
          <graphic xlink:href="https://amt.copernicus.org/articles/18/1243/2025/amt-18-1243-2025-f03.png"/>

        </fig>


</sec>
<sec id="Ch1.S3.SS2">
  <label>3.2</label><title>Optimization of the FRS system</title>
      <p id="d2e2411">For weak absorption, the FRS signal (<inline-formula><mml:math id="M169" display="inline"><mml:mrow><mml:msub><mml:mi>S</mml:mi><mml:mtext>FRS</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) and total noise (<inline-formula><mml:math id="M170" display="inline"><mml:mrow><mml:msub><mml:mi>N</mml:mi><mml:mtext>tot</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) of the system can be expressed as functions of the analyser offset angle (<inline-formula><mml:math id="M171" display="inline"><mml:mi mathvariant="italic">ϕ</mml:mi></mml:math></inline-formula>) from the crossed polarization of the light (Zhao et al., 2011; Wei et al., 2020):

                <disp-formula specific-use="align" content-type="numbered"><mml:math id="M172" display="block"><mml:mtable displaystyle="true"><mml:mlabeledtr id="Ch1.E3"><mml:mtd><mml:mtext>3</mml:mtext></mml:mtd><mml:mtd><mml:mstyle class="stylechange" displaystyle="true"/></mml:mtd><mml:mtd><mml:mrow><mml:mstyle displaystyle="true" class="stylechange"/><mml:msub><mml:mi>S</mml:mi><mml:mtext>FRS</mml:mtext></mml:msub><mml:mo>(</mml:mo><mml:mi mathvariant="italic">ν</mml:mi><mml:mo>)</mml:mo><mml:mo>=</mml:mo><mml:mi mathvariant="italic">γ</mml:mi><mml:mi>N</mml:mi><mml:mi>S</mml:mi><mml:msub><mml:mtext>LP</mml:mtext><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mi>sin⁡</mml:mi><mml:mo>(</mml:mo><mml:mn mathvariant="normal">2</mml:mn><mml:mi mathvariant="italic">ϕ</mml:mi><mml:mo>)</mml:mo><mml:mi mathvariant="italic">χ</mml:mi><mml:mo>(</mml:mo><mml:mi mathvariant="italic">ν</mml:mi><mml:mo>)</mml:mo><mml:mo>,</mml:mo></mml:mrow></mml:mtd></mml:mlabeledtr><mml:mlabeledtr id="Ch1.E4"><mml:mtd><mml:mtext>4</mml:mtext></mml:mtd><mml:mtd><mml:mstyle class="stylechange" displaystyle="true"/></mml:mtd><mml:mtd><mml:mrow><mml:mstyle class="stylechange" displaystyle="true"/><mml:msub><mml:mi>N</mml:mi><mml:mtext>tot</mml:mtext></mml:msub><mml:mo>(</mml:mo><mml:mi mathvariant="italic">ϕ</mml:mi><mml:mo>)</mml:mo><mml:mo>=</mml:mo><mml:msqrt><mml:mtable class="array" columnalign="center"><mml:mtr><mml:mtd><mml:mrow><mml:msubsup><mml:mi>N</mml:mi><mml:mn mathvariant="normal">0</mml:mn><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup><mml:mo>+</mml:mo><mml:msup><mml:mfenced close=")" open="("><mml:mrow><mml:msub><mml:mi>N</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:msqrt><mml:mrow><mml:mo>(</mml:mo><mml:msup><mml:mi>sin⁡</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:mo>(</mml:mo><mml:mi mathvariant="italic">ϕ</mml:mi><mml:mo>)</mml:mo><mml:mo>+</mml:mo><mml:mi mathvariant="italic">ξ</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:msqrt></mml:mrow></mml:mfenced><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow><mml:mo>+</mml:mo><mml:msup><mml:mfenced close=")" open="("><mml:mrow><mml:msub><mml:mi>N</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mo>(</mml:mo><mml:msup><mml:mi>sin⁡</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:mo>(</mml:mo><mml:mi mathvariant="italic">ϕ</mml:mi><mml:mo>)</mml:mo><mml:mo>+</mml:mo><mml:mi mathvariant="italic">ξ</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:mfenced><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:mo>,</mml:mo></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:msqrt></mml:mrow></mml:mtd></mml:mlabeledtr></mml:mtable></mml:math></disp-formula>

            where <inline-formula><mml:math id="M173" display="inline"><mml:mi mathvariant="italic">ν</mml:mi></mml:math></inline-formula> is the laser frequency, <inline-formula><mml:math id="M174" display="inline"><mml:mi mathvariant="italic">γ</mml:mi></mml:math></inline-formula> is the instrumentation factor, <inline-formula><mml:math id="M175" display="inline"><mml:mi>N</mml:mi></mml:math></inline-formula> is the OH concentration, <inline-formula><mml:math id="M176" display="inline"><mml:mi>S</mml:mi></mml:math></inline-formula> is the absorption line strength of OH, and <inline-formula><mml:math id="M177" display="inline"><mml:mi mathvariant="italic">χ</mml:mi></mml:math></inline-formula> is the Faraday rotation line shape (Westberg and Axner, 2014). <inline-formula><mml:math id="M178" display="inline"><mml:mrow><mml:msub><mml:mi>N</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M179" display="inline"><mml:mrow><mml:msub><mml:mi>N</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:msqrt><mml:mrow><mml:mo>(</mml:mo><mml:msup><mml:mi>sin⁡</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:mo>(</mml:mo><mml:mi mathvariant="italic">ϕ</mml:mi><mml:mo>)</mml:mo><mml:mo>+</mml:mo><mml:mi mathvariant="italic">ξ</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:msqrt></mml:mrow></mml:math></inline-formula>, and <inline-formula><mml:math id="M180" display="inline"><mml:mrow><mml:msub><mml:mi>N</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mo>(</mml:mo><mml:msup><mml:mi>sin⁡</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:mo>(</mml:mo><mml:mi mathvariant="italic">ϕ</mml:mi><mml:mo>)</mml:mo><mml:mo>+</mml:mo><mml:mi mathvariant="italic">ξ</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula> are the detector noise, shot noise, and laser noise of the system, respectively. It is noted that the FRS signal reaches its maximum value when <inline-formula><mml:math id="M181" display="inline"><mml:mi mathvariant="italic">ϕ</mml:mi></mml:math></inline-formula> <inline-formula><mml:math id="M182" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula>  <inline-formula><mml:math id="M183" display="inline"><mml:mo>±</mml:mo></mml:math></inline-formula> 45°, while the total noise is more sensitive to <inline-formula><mml:math id="M184" display="inline"><mml:mrow><mml:msup><mml:mi>sin⁡</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:mo>(</mml:mo><mml:mi mathvariant="italic">ϕ</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula>. The maximum signal-to-noise ratio (SNR) usually occurs at a small offset angle, which depends on system noise (Lewicki et al., 2009).</p>
      <p id="d2e2754">The total noises at various offset angles and the detector noise were measured with the lock-in amplifier to determine the noise sources and the optimum angle (<inline-formula><mml:math id="M185" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">ϕ</mml:mi><mml:mtext>opt</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) for maximizing the SNR of the FRS system (Zhao et al., 2011). Figure <xref ref-type="fig" rid="Ch1.F3"/>a shows a fit analysis of the data using Eq. (<xref ref-type="disp-formula" rid="Ch1.E4"/>). For offset angles below 5.5°, detector noise is the main noise of the system. The measured detector noise was 300 <inline-formula><mml:math id="M186" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">nV</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">Hz</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn><mml:mo>/</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, which closely agreed with the manufacturer's specified value of 290 <inline-formula><mml:math id="M187" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">nV</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">Hz</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn><mml:mo>/</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>. Laser noise dominates and rapidly increases beyond an offset angle greater than 11.5°. Since the FRS signal is proportional to <inline-formula><mml:math id="M188" display="inline"><mml:mrow><mml:mi>sin⁡</mml:mi><mml:mo>(</mml:mo><mml:mn mathvariant="normal">2</mml:mn><mml:mi mathvariant="italic">ϕ</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula>, the relative SNR for a given absorption at a fixed laser frequency can be evaluated from <inline-formula><mml:math id="M189" display="inline"><mml:mrow><mml:mrow class="chem"><mml:mi mathvariant="normal">SNR</mml:mi></mml:mrow><mml:mo>∝</mml:mo><mml:mi>sin⁡</mml:mi><mml:mo>(</mml:mo><mml:mn mathvariant="normal">2</mml:mn><mml:mi mathvariant="italic">ϕ</mml:mi><mml:mo>)</mml:mo><mml:mo>/</mml:mo><mml:msub><mml:mi>N</mml:mi><mml:mtext>tot</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>. As shown in Fig. <xref ref-type="fig" rid="Ch1.F3"/>b, the SNR of our system peaks at the <inline-formula><mml:math id="M190" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">ϕ</mml:mi><mml:mtext>opt</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> of <inline-formula><mml:math id="M191" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 8°. At this angle, the laser noise was suppressed to 310 <inline-formula><mml:math id="M192" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">nV</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">Hz</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn><mml:mo>/</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, equivalent to the detector noise level. The total system noise was 610 <inline-formula><mml:math id="M193" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">nV</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">Hz</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn><mml:mo>/</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, which was 1.4 times higher than the measured shot noise of 440 <inline-formula><mml:math id="M194" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">nV</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">Hz</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn><mml:mo>/</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>.</p>

      <fig id="Ch1.F4"><label>Figure 4</label><caption><p id="d2e2945">FRS signal intensity as functions of the <bold>(a)</bold> modulation amplitude and <bold>(b)</bold> current of the coil. The optimum modulation amplitude and magnetic field strength are 360 <inline-formula><mml:math id="M195" display="inline"><mml:mrow class="unit"><mml:msub><mml:mi mathvariant="normal">mV</mml:mi><mml:mi mathvariant="normal">rms</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> and 307 <inline-formula><mml:math id="M196" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">G</mml:mi></mml:mrow></mml:math></inline-formula>, respectively.</p></caption>
          <graphic xlink:href="https://amt.copernicus.org/articles/18/1243/2025/amt-18-1243-2025-f04.png"/>

        </fig>

      <p id="d2e2980">In this work, the magnetic circular birefringence of OH was effectively modulated with wavelength modulation in a static magnetic field generated by the DC coil. The modulation amplitude and magnetic field strength are critical parameters that affect the intensity of the demodulated FRS signal (Zhao et al., 2018; Fang et al., 2020). The theoretical optimum modulation amplitude is 2.2 times the half-width at half-maximum (HWHM) of the absorption line shape (Schilt et al., 2003). The optimum magnetic field strength (<inline-formula><mml:math id="M197" display="inline"><mml:mrow><mml:msub><mml:mi>B</mml:mi><mml:mtext>opt</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) is the value that can make the Zeeman splitting comparable with the HWHM (Brecha et al., 1997). A direct and effective approach for determining the two optimum parameters is recording the signal intensity values under series amplitudes of the sinusoidal wave output from the lock-in amplifier and different coil currents. As shown in Fig. <xref ref-type="fig" rid="Ch1.F4"/>, the FRS signal intensity value is calculated from the difference before and after the laser flash. The maximum intensity occurred at an amplitude of 360 <inline-formula><mml:math id="M198" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">mV</mml:mi></mml:mrow></mml:math></inline-formula> and a coil current of 4.2 <inline-formula><mml:math id="M199" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">A</mml:mi></mml:mrow></mml:math></inline-formula>, which corresponds to a wavelength modulation amplitude of <inline-formula><mml:math id="M200" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 0.048 <inline-formula><mml:math id="M201" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> (<inline-formula><mml:math id="M202" display="inline"><mml:mo lspace="0mm">∼</mml:mo></mml:math></inline-formula> 2.45 times the calculated OH absorption linewidth of <inline-formula><mml:math id="M203" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 0.020 <inline-formula><mml:math id="M204" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> in air) and a <inline-formula><mml:math id="M205" display="inline"><mml:mrow><mml:msub><mml:mi>B</mml:mi><mml:mtext>opt</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> of 307 <inline-formula><mml:math id="M206" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">G</mml:mi></mml:mrow></mml:math></inline-formula>, respectively.</p>
</sec>
<sec id="Ch1.S3.SS3">
  <label>3.3</label><title>OH concentration in the cell</title>
      <p id="d2e3089">To produce sufficient OH in the MPC, a small flow rate (<inline-formula><mml:math id="M207" display="inline"><mml:mo lspace="0mm">∼</mml:mo></mml:math></inline-formula> 0.25 <inline-formula><mml:math id="M208" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">L</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">min</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>) of zero air, which passed through a UV lamp (UVP Pen-Ray, Analytik Jena) and a bubbling bottle to generate <inline-formula><mml:math id="M209" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and water vapour, is added to the main sampling flow (<inline-formula><mml:math id="M210" display="inline"><mml:mo lspace="0mm">∼</mml:mo></mml:math></inline-formula> 6.0 <inline-formula><mml:math id="M211" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">L</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">min</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>), resulting in a total flow rate of 6.25 <inline-formula><mml:math id="M212" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">L</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">min</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>. The operation pressure in the MPC is set to 200 <inline-formula><mml:math id="M213" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">mbar</mml:mi></mml:mrow></mml:math></inline-formula> and maintained by a butterfly valve (DN40, VAT). The flow velocity in the cell is 27 <inline-formula><mml:math id="M214" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, corresponding to a Reynolds number of <inline-formula><mml:math id="M215" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 170, which met the laminar flow condition. OH is produced by the 266 <inline-formula><mml:math id="M216" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">nm</mml:mi></mml:mrow></mml:math></inline-formula> laser photolysis of <inline-formula><mml:math id="M217" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and then followed by reaction of <inline-formula><mml:math id="M218" display="inline"><mml:mrow class="chem"><mml:mi mathvariant="normal">O</mml:mi><mml:msup><mml:mo>(</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:msup><mml:mi mathvariant="normal">D</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula> with water vapour (Sadanaga et al., 2004): 

                <disp-formula specific-use="align" content-type="numbered reaction"><mml:math id="M219" display="block"><mml:mtable displaystyle="true"><mml:mlabeledtr id="Ch1.R5"><mml:mtd><mml:mtext>R1</mml:mtext></mml:mtd><mml:mtd><mml:mstyle displaystyle="true" class="stylechange"/></mml:mtd><mml:mtd><mml:mrow><mml:mstyle class="stylechange" displaystyle="true"/><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow><mml:mo>+</mml:mo><mml:mi>h</mml:mi><mml:mi>v</mml:mi><mml:mo>(</mml:mo><mml:mi mathvariant="italic">λ</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">266</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mrow class="unit"><mml:mi mathvariant="normal">nm</mml:mi></mml:mrow><mml:mo>)</mml:mo><mml:mo>→</mml:mo><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow><mml:mo>+</mml:mo><mml:mrow class="chem"><mml:mi mathvariant="normal">O</mml:mi><mml:msup><mml:mo>(</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:msup><mml:mi mathvariant="normal">D</mml:mi><mml:mo>)</mml:mo></mml:mrow><mml:mo>,</mml:mo></mml:mrow></mml:mtd></mml:mlabeledtr><mml:mlabeledtr id="Ch1.R6"><mml:mtd><mml:mtext>R2</mml:mtext></mml:mtd><mml:mtd><mml:mstyle class="stylechange" displaystyle="true"/></mml:mtd><mml:mtd><mml:mrow><mml:mstyle class="stylechange" displaystyle="true"/><mml:mrow class="chem"><mml:mi mathvariant="normal">O</mml:mi><mml:msup><mml:mo>(</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:msup><mml:mi mathvariant="normal">D</mml:mi><mml:mo>)</mml:mo></mml:mrow><mml:mo>+</mml:mo><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mi mathvariant="normal">O</mml:mi></mml:mrow><mml:mo>→</mml:mo><mml:mn mathvariant="normal">2</mml:mn><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>.</mml:mo></mml:mrow></mml:mtd></mml:mlabeledtr></mml:mtable></mml:math></disp-formula></p>
      <p id="d2e3345">The concentrations of <inline-formula><mml:math id="M220" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and the water vapour directly influence the OH produced. A dew point sensor was used to measure the water vapour mixing ratio of the total flow. Based on the Magnus–Tetens formula (Lawrence, 2005), the absolute water vapour mass concentration can be evaluated from <inline-formula><mml:math id="M221" display="inline"><mml:mrow><mml:mi mathvariant="italic">ρ</mml:mi><mml:mo>(</mml:mo><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mi mathvariant="normal">O</mml:mi></mml:mrow><mml:mo>)</mml:mo><mml:mo>=</mml:mo><mml:mi>e</mml:mi><mml:mo>/</mml:mo><mml:mo>(</mml:mo><mml:msub><mml:mi>R</mml:mi><mml:mi mathvariant="normal">w</mml:mi></mml:msub><mml:mo>⋅</mml:mo><mml:mi>T</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula>, where <inline-formula><mml:math id="M222" display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mi mathvariant="normal">w</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M223" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 461.52 <inline-formula><mml:math id="M224" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">J</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mo>(</mml:mo><mml:mi mathvariant="normal">kg</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mi mathvariant="normal">K</mml:mi><mml:msup><mml:mo>)</mml:mo><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M225" display="inline"><mml:mi>T</mml:mi></mml:math></inline-formula> is the sample temperature, <inline-formula><mml:math id="M226" display="inline"><mml:mrow><mml:mi>e</mml:mi><mml:mo>=</mml:mo><mml:mi>C</mml:mi><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>(</mml:mo><mml:mi>A</mml:mi><mml:mo>⋅</mml:mo><mml:msub><mml:mi>T</mml:mi><mml:mi mathvariant="normal">d</mml:mi></mml:msub><mml:mo>/</mml:mo><mml:mo>(</mml:mo><mml:mi>B</mml:mi><mml:mo>+</mml:mo><mml:msub><mml:mi>T</mml:mi><mml:mi mathvariant="normal">d</mml:mi></mml:msub><mml:mo>)</mml:mo><mml:mo>)</mml:mo></mml:mrow></mml:msup><mml:mo>⋅</mml:mo><mml:mo>(</mml:mo><mml:mi>P</mml:mi><mml:mo>/</mml:mo><mml:msub><mml:mi>P</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula> is the actual water vapour pressure at a current pressure of <inline-formula><mml:math id="M227" display="inline"><mml:mi>P</mml:mi></mml:math></inline-formula>, <inline-formula><mml:math id="M228" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula> <inline-formula><mml:math id="M229" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 17.625, <inline-formula><mml:math id="M230" display="inline"><mml:mi>B</mml:mi></mml:math></inline-formula> <inline-formula><mml:math id="M231" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 243.04 <inline-formula><mml:math id="M232" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">°</mml:mi><mml:mi mathvariant="normal">C</mml:mi></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M233" display="inline"><mml:mi>C</mml:mi></mml:math></inline-formula> <inline-formula><mml:math id="M234" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 610.94 <inline-formula><mml:math id="M235" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">Pa</mml:mi></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M236" display="inline"><mml:mrow><mml:msub><mml:mi>P</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> is the standard atmospheric pressure, and <inline-formula><mml:math id="M237" display="inline"><mml:mrow><mml:msub><mml:mi>T</mml:mi><mml:mi mathvariant="normal">d</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> is the measured dew point temperature. The calculated water vapour volume concentration was <inline-formula><mml:math id="M238" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 0.13 % when using zero air for the system test, while it increased to <inline-formula><mml:math id="M239" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 1.5 % when measuring the real atmosphere. The <inline-formula><mml:math id="M240" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> concentration is estimated by measuring the energy of the photolysis laser pulse with the UV lamp on and off. Only about 0.3 % of the pulse energy was absorbed by <inline-formula><mml:math id="M241" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>. Based on the Beer–Lambert law and the <inline-formula><mml:math id="M242" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> absorption cross section of <inline-formula><mml:math id="M243" display="inline"><mml:mi mathvariant="italic">σ</mml:mi></mml:math></inline-formula> <inline-formula><mml:math id="M244" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 9.65 <inline-formula><mml:math id="M245" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<sup>−18</sup> <inline-formula><mml:math id="M247" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:mrow></mml:math></inline-formula> at 266 <inline-formula><mml:math id="M248" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">nm</mml:mi></mml:mrow></mml:math></inline-formula> (Sadanaga et al., 2004), the <inline-formula><mml:math id="M249" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> concentration is determined to be <inline-formula><mml:math id="M250" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 800 <inline-formula><mml:math id="M251" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">ppbv</mml:mi></mml:mrow></mml:math></inline-formula>. The recommended quantum yield of the <inline-formula><mml:math id="M252" display="inline"><mml:mrow class="chem"><mml:mi mathvariant="normal">O</mml:mi><mml:msup><mml:mo>(</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:msup><mml:mi mathvariant="normal">D</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula> produced by laser-flash photolysis is <inline-formula><mml:math id="M253" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 0.9 (Atkinson et al., 2004), resulting in <inline-formula><mml:math id="M254" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 2.2 <inline-formula><mml:math id="M255" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<sup>11</sup> <inline-formula><mml:math id="M257" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">molec</mml:mi><mml:mo>.</mml:mo><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> of <inline-formula><mml:math id="M258" display="inline"><mml:mrow class="chem"><mml:mi mathvariant="normal">O</mml:mi><mml:msup><mml:mo>(</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:msup><mml:mi mathvariant="normal">D</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula>. The number density of OH produced by each <inline-formula><mml:math id="M259" display="inline"><mml:mrow class="chem"><mml:mi mathvariant="normal">O</mml:mi><mml:msup><mml:mo>(</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:msup><mml:mi mathvariant="normal">D</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula> can be estimated by (Wei et al., 2020) 
            <disp-formula id="Ch1.E7" content-type="numbered"><label>5</label><mml:math id="M260" display="block"><mml:mrow><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">OH</mml:mi><mml:mo>]</mml:mo></mml:mrow><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mn mathvariant="normal">2</mml:mn><mml:msub><mml:mi>k</mml:mi><mml:mn mathvariant="normal">6</mml:mn></mml:msub><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">O</mml:mi><mml:msup><mml:mo>(</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:msup><mml:mi mathvariant="normal">D</mml:mi><mml:mo>)</mml:mo><mml:mo>]</mml:mo></mml:mrow><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mo>]</mml:mo></mml:mrow></mml:mrow><mml:mrow><mml:mo>(</mml:mo><mml:msub><mml:mi>k</mml:mi><mml:mn mathvariant="normal">5</mml:mn></mml:msub><mml:mo>[</mml:mo><mml:mi>M</mml:mi><mml:mo>]</mml:mo><mml:mo>+</mml:mo><mml:msub><mml:mi>k</mml:mi><mml:mn mathvariant="normal">6</mml:mn></mml:msub><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mo>]</mml:mo></mml:mrow><mml:mo>)</mml:mo><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">O</mml:mi><mml:msup><mml:mo>(</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:msup><mml:mi mathvariant="normal">D</mml:mi><mml:mo>)</mml:mo><mml:mo>]</mml:mo></mml:mrow></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>≅</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mn mathvariant="normal">2</mml:mn><mml:msub><mml:mi>k</mml:mi><mml:mn mathvariant="normal">6</mml:mn></mml:msub></mml:mrow><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mn mathvariant="normal">5</mml:mn></mml:msub></mml:mrow></mml:mfrac></mml:mstyle><mml:msub><mml:mi mathvariant="italic">χ</mml:mi><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mi mathvariant="normal">O</mml:mi></mml:mrow></mml:msub><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where <inline-formula><mml:math id="M261" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">OH</mml:mi><mml:mo>]</mml:mo></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M262" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:mi mathvariant="normal">O</mml:mi><mml:msup><mml:mo>(</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:msup><mml:mi mathvariant="normal">D</mml:mi><mml:mo>)</mml:mo><mml:mo>]</mml:mo></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M263" display="inline"><mml:mrow class="chem"><mml:mo>[</mml:mo><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mo>]</mml:mo></mml:mrow></mml:math></inline-formula>, and <inline-formula><mml:math id="M264" display="inline"><mml:mrow><mml:mo>[</mml:mo><mml:mi>M</mml:mi><mml:mo>]</mml:mo></mml:mrow></mml:math></inline-formula> represent the number densities of the corresponding molecule. <inline-formula><mml:math id="M265" display="inline"><mml:mi>M</mml:mi></mml:math></inline-formula> is the “bath” gas during the chemical reaction of OH formation. <inline-formula><mml:math id="M266" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">χ</mml:mi><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mi mathvariant="normal">O</mml:mi></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula> is the volume concentration of water vapour. <inline-formula><mml:math id="M267" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mn mathvariant="normal">5</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M268" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mn mathvariant="normal">6</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> are 2.9 <inline-formula><mml:math id="M269" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<sup>−11</sup> and 2.2 <inline-formula><mml:math id="M271" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<sup>−10</sup> <inline-formula><mml:math id="M273" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msup><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mi mathvariant="normal">molec</mml:mi><mml:msup><mml:mo>.</mml:mo><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> at 298 <inline-formula><mml:math id="M274" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">K</mml:mi></mml:mrow></mml:math></inline-formula>, respectively. The concentration of OH produced in the cell was <inline-formula><mml:math id="M275" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 4.3 <inline-formula><mml:math id="M276" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<sup>9</sup> <inline-formula><mml:math id="M278" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">molec</mml:mi><mml:mo>.</mml:mo><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> during the system test and <inline-formula><mml:math id="M279" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 5 <inline-formula><mml:math id="M280" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<sup>10</sup> <inline-formula><mml:math id="M282" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">molec</mml:mi><mml:mo>.</mml:mo><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> during the field application due to different <inline-formula><mml:math id="M283" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">χ</mml:mi><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mi mathvariant="normal">O</mml:mi></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula> in the sample.</p>
</sec>
<sec id="Ch1.S3.SS4">
  <label>3.4</label><title>Kinetics test</title>
      <p id="d2e4264">The performance of the LP-FRS instrument in measuring different reaction rates was verified with three well-known reactions (Wei et al., 2020; Yan et al., 2020). Reactants from the cylinders (i.e. <inline-formula><mml:math id="M284" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">CH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> (99.999 %, Nanjingteqi), CO (2.01 %, Nanjingteqi), and NO (100 <inline-formula><mml:math id="M285" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">ppmv</mml:mi></mml:mrow></mml:math></inline-formula>, Linde)) were added to the main flow at different flow rates. When the concentrations of reactants are much higher than those of OH, the OH decay rate (<inline-formula><mml:math id="M286" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mtext>decay</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) follows pseudo-first-order kinetics and can be determined by fitting the measured decay spectra to the following exponential equation:
            <disp-formula id="Ch1.E8" content-type="numbered"><label>6</label><mml:math id="M287" display="block"><mml:mrow><mml:msub><mml:mi>S</mml:mi><mml:mi>t</mml:mi></mml:msub><mml:mo>=</mml:mo><mml:msub><mml:mi>S</mml:mi><mml:mtext>background</mml:mtext></mml:msub><mml:mo>+</mml:mo><mml:msub><mml:mi>S</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mi>exp⁡</mml:mi><mml:mo>(</mml:mo><mml:mo>-</mml:mo><mml:msub><mml:mi>k</mml:mi><mml:mtext>decay</mml:mtext></mml:msub><mml:mi>t</mml:mi><mml:mo>)</mml:mo><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where <inline-formula><mml:math id="M288" display="inline"><mml:mrow><mml:msub><mml:mi>S</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M289" display="inline"><mml:mrow><mml:msub><mml:mi>S</mml:mi><mml:mi>t</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> are the FRS signal intensities proportional to the OH concentration at the time when the fitting started and at the time <inline-formula><mml:math id="M290" display="inline"><mml:mi>t</mml:mi></mml:math></inline-formula>, respectively. <inline-formula><mml:math id="M291" display="inline"><mml:mrow><mml:msub><mml:mi>S</mml:mi><mml:mtext>background</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> is the background signal intensity. Since the fitted values for <inline-formula><mml:math id="M292" display="inline"><mml:mi>y</mml:mi></mml:math></inline-formula> and <inline-formula><mml:math id="M293" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mtext>decay</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> do not depend on the selected time period of the decay curve (Stone et al., 2016), the fit is started at the time of 36 <inline-formula><mml:math id="M294" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">ms</mml:mi></mml:mrow></mml:math></inline-formula> rather than the peak to avoid any fluctuations affecting the fitting result. Figure <xref ref-type="fig" rid="Ch1.F5"/> shows two typical decays with loss rates of <inline-formula><mml:math id="M295" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mtext>decay</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M296" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 8.4 <inline-formula><mml:math id="M297" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M298" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mtext>decay</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M299" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 50.2 <inline-formula><mml:math id="M300" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, which are given with a 60 <inline-formula><mml:math id="M301" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">s</mml:mi></mml:mrow></mml:math></inline-formula> averaging time during the measurements. The recorded time-resolved decay spectra clearly depict the entire event, including the baseline, the instant generation of OH by laser photolysis, and the decay process.</p>

      <fig id="Ch1.F5"><label>Figure 5</label><caption><p id="d2e4485">Two typical OH decay spectra with different loss rates. Time zero is defined as the moment when the data acquisition trigger occurs.</p></caption>
          <graphic xlink:href="https://amt.copernicus.org/articles/18/1243/2025/amt-18-1243-2025-f05.png"/>

        </fig>

      <fig id="Ch1.F6" specific-use="star"><label>Figure 6</label><caption><p id="d2e4496">Plots of the measured pseudo-first-order rate coefficients vs. <bold>(a)</bold> <inline-formula><mml:math id="M302" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">CH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> concentrations, <bold>(b)</bold> CO concentrations, and <bold>(c)</bold> NO at 298 <inline-formula><mml:math id="M303" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">K</mml:mi></mml:mrow></mml:math></inline-formula>. The measured reaction rate constants obtained from the slopes are <inline-formula><mml:math id="M304" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mrow><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>+</mml:mo><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">CH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub></mml:mrow></mml:mrow></mml:msub><mml:mo>=</mml:mo><mml:msubsup><mml:mn mathvariant="normal">6.4</mml:mn><mml:mrow><mml:mo>+</mml:mo><mml:mn mathvariant="normal">0.1</mml:mn></mml:mrow><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.1</mml:mn></mml:mrow></mml:msubsup><mml:mo>×</mml:mo></mml:mrow></mml:math></inline-formula> 10<sup>−15</sup>, <inline-formula><mml:math id="M306" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mrow><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>+</mml:mo><mml:mrow class="chem"><mml:mi mathvariant="normal">CO</mml:mi></mml:mrow></mml:mrow></mml:msub><mml:mo>=</mml:mo><mml:msubsup><mml:mn mathvariant="normal">1.6</mml:mn><mml:mrow><mml:mo>+</mml:mo><mml:mn mathvariant="normal">0.1</mml:mn></mml:mrow><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.1</mml:mn></mml:mrow></mml:msubsup><mml:mo>×</mml:mo></mml:mrow></mml:math></inline-formula> 10<sup>−13</sup>, and <inline-formula><mml:math id="M308" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mrow><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>+</mml:mo><mml:mrow class="chem"><mml:mi mathvariant="normal">NO</mml:mi></mml:mrow></mml:mrow></mml:msub><mml:mo>=</mml:mo><mml:msubsup><mml:mn mathvariant="normal">3.0</mml:mn><mml:mrow><mml:mo>+</mml:mo><mml:mn mathvariant="normal">0.1</mml:mn></mml:mrow><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.1</mml:mn></mml:mrow></mml:msubsup><mml:mo>×</mml:mo></mml:mrow></mml:math></inline-formula> 10<sup>−12</sup> <inline-formula><mml:math id="M310" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msup><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi mathvariant="normal">molec</mml:mi><mml:msup><mml:mo>.</mml:mo><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, which agree with the recommended values of <inline-formula><mml:math id="M311" display="inline"><mml:mrow><mml:msubsup><mml:mn mathvariant="normal">6.4</mml:mn><mml:mrow><mml:mo>+</mml:mo><mml:mn mathvariant="normal">1.3</mml:mn></mml:mrow><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1.1</mml:mn></mml:mrow></mml:msubsup><mml:mo>×</mml:mo></mml:mrow></mml:math></inline-formula> 10<sup>−15</sup>, <inline-formula><mml:math id="M313" display="inline"><mml:mrow><mml:msubsup><mml:mn mathvariant="normal">1.6</mml:mn><mml:mrow><mml:mo>+</mml:mo><mml:mn mathvariant="normal">0.2</mml:mn></mml:mrow><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.2</mml:mn></mml:mrow></mml:msubsup><mml:mo>×</mml:mo></mml:mrow></mml:math></inline-formula> 10<sup>−13</sup>, and <inline-formula><mml:math id="M315" display="inline"><mml:mrow><mml:msubsup><mml:mn mathvariant="normal">3.0</mml:mn><mml:mrow><mml:mo>+</mml:mo><mml:mn mathvariant="normal">0.8</mml:mn></mml:mrow><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.6</mml:mn></mml:mrow></mml:msubsup><mml:mo>×</mml:mo></mml:mrow></mml:math></inline-formula> 10<sup>−12</sup> <inline-formula><mml:math id="M317" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msup><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi mathvariant="normal">molec</mml:mi><mml:msup><mml:mo>.</mml:mo><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, respectively.</p></caption>
          <graphic xlink:href="https://amt.copernicus.org/articles/18/1243/2025/amt-18-1243-2025-f06.png"/>

        </fig>

      <p id="d2e4842">The OH decay rates in the reactions with three different species were measured and can be expressed as <inline-formula><mml:math id="M318" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mtext>decay</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:msub><mml:mi>k</mml:mi><mml:mrow><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>+</mml:mo><mml:mi>X</mml:mi></mml:mrow></mml:msub><mml:mo>[</mml:mo><mml:mi>X</mml:mi><mml:mo>]</mml:mo><mml:mo>+</mml:mo><mml:msub><mml:mi>k</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, where <inline-formula><mml:math id="M319" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mrow><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>+</mml:mo><mml:mi>X</mml:mi></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula> is the measured rate constant for the reaction of OH with <inline-formula><mml:math id="M320" display="inline"><mml:mi>X</mml:mi></mml:math></inline-formula>, <inline-formula><mml:math id="M321" display="inline"><mml:mrow><mml:mo>[</mml:mo><mml:mi>X</mml:mi><mml:mo>]</mml:mo></mml:mrow></mml:math></inline-formula> is the concentration of reactant <inline-formula><mml:math id="M322" display="inline"><mml:mi>X</mml:mi></mml:math></inline-formula>, and <inline-formula><mml:math id="M323" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> is a background value. As shown in Fig. <xref ref-type="fig" rid="Ch1.F6"/>, the obtained reaction rate constants for OH <inline-formula><mml:math id="M324" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula> <inline-formula><mml:math id="M325" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">CH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, OH <inline-formula><mml:math id="M326" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula> CO, and OH <inline-formula><mml:math id="M327" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula> NO at 298 <inline-formula><mml:math id="M328" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">K</mml:mi></mml:mrow></mml:math></inline-formula> were found to be <inline-formula><mml:math id="M329" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mrow><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>+</mml:mo><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">CH</mml:mi><mml:mn mathvariant="normal">4</mml:mn></mml:msub></mml:mrow></mml:mrow></mml:msub><mml:mo>=</mml:mo><mml:msubsup><mml:mn mathvariant="normal">6.4</mml:mn><mml:mrow><mml:mo>+</mml:mo><mml:mn mathvariant="normal">0.1</mml:mn></mml:mrow><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.1</mml:mn></mml:mrow></mml:msubsup><mml:mo>×</mml:mo></mml:mrow></mml:math></inline-formula> 10<sup>−15</sup>, <inline-formula><mml:math id="M331" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mrow><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>+</mml:mo><mml:mrow class="chem"><mml:mi mathvariant="normal">CO</mml:mi></mml:mrow></mml:mrow></mml:msub><mml:mo>=</mml:mo><mml:msubsup><mml:mn mathvariant="normal">1.6</mml:mn><mml:mrow><mml:mo>+</mml:mo><mml:mn mathvariant="normal">0.1</mml:mn></mml:mrow><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.1</mml:mn></mml:mrow></mml:msubsup><mml:mo>×</mml:mo></mml:mrow></mml:math></inline-formula> 10<sup>−13</sup>, and <inline-formula><mml:math id="M333" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mrow><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>+</mml:mo><mml:mrow class="chem"><mml:mi mathvariant="normal">NO</mml:mi></mml:mrow></mml:mrow></mml:msub><mml:mo>=</mml:mo><mml:msubsup><mml:mn mathvariant="normal">3.0</mml:mn><mml:mrow><mml:mo>+</mml:mo><mml:mn mathvariant="normal">0.1</mml:mn></mml:mrow><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.1</mml:mn></mml:mrow></mml:msubsup><mml:mo>×</mml:mo></mml:mrow></mml:math></inline-formula> 10<sup>−12</sup> <inline-formula><mml:math id="M335" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msup><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi mathvariant="normal">molec</mml:mi><mml:msup><mml:mo>.</mml:mo><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, respectively. The measured values are in agreement with the International Union of Pure and Applied Chemistry (IUPAC) recommended values of <inline-formula><mml:math id="M336" display="inline"><mml:mrow><mml:msubsup><mml:mn mathvariant="normal">6.4</mml:mn><mml:mrow><mml:mo>+</mml:mo><mml:mn mathvariant="normal">1.3</mml:mn></mml:mrow><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1.1</mml:mn></mml:mrow></mml:msubsup><mml:mo>×</mml:mo></mml:mrow></mml:math></inline-formula> 10<sup>−15</sup>, <inline-formula><mml:math id="M338" display="inline"><mml:mrow><mml:msubsup><mml:mn mathvariant="normal">1.6</mml:mn><mml:mrow><mml:mo>+</mml:mo><mml:mn mathvariant="normal">0.2</mml:mn></mml:mrow><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.2</mml:mn></mml:mrow></mml:msubsup><mml:mo>×</mml:mo></mml:mrow></mml:math></inline-formula> 10<sup>−13</sup>, and <inline-formula><mml:math id="M340" display="inline"><mml:mrow><mml:msubsup><mml:mn mathvariant="normal">3.0</mml:mn><mml:mrow><mml:mo>+</mml:mo><mml:mn mathvariant="normal">0.8</mml:mn></mml:mrow><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0.6</mml:mn></mml:mrow></mml:msubsup><mml:mo>×</mml:mo></mml:mrow></mml:math></inline-formula> 10<sup>−12</sup> <inline-formula><mml:math id="M342" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msup><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mi mathvariant="normal">molec</mml:mi><mml:msup><mml:mo>.</mml:mo><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, respectively (Atkinson et al., 2004, 2006).</p>
</sec>
<sec id="Ch1.S3.SS5">
  <label>3.5</label><title>Precision and uncertainty of <inline-formula><mml:math id="M343" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> measurement</title>
      <p id="d2e5311">When the LP-FRS instrument is used for measuring atmospheric <inline-formula><mml:math id="M344" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula>, the fitted <inline-formula><mml:math id="M345" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mtext>decay</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> value requires corrections for dilution and instrument zero (<inline-formula><mml:math id="M346" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mtext>zero</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>). Incorporating these corrections, the atmospheric <inline-formula><mml:math id="M347" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> is expressed as
            <disp-formula id="Ch1.E9" content-type="numbered"><label>7</label><mml:math id="M348" display="block"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup><mml:mo>=</mml:mo><mml:mi>f</mml:mi><mml:mo>×</mml:mo><mml:mo>(</mml:mo><mml:msub><mml:mi>k</mml:mi><mml:mtext>decay</mml:mtext></mml:msub><mml:mo>-</mml:mo><mml:msub><mml:mi>k</mml:mi><mml:mtext>zero</mml:mtext></mml:msub><mml:mo>)</mml:mo><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where <inline-formula><mml:math id="M349" display="inline"><mml:mi>f</mml:mi></mml:math></inline-formula>, given by <inline-formula><mml:math id="M350" display="inline"><mml:mrow><mml:mi>f</mml:mi><mml:mo>=</mml:mo><mml:msub><mml:mi>f</mml:mi><mml:mtext>pressure</mml:mtext></mml:msub><mml:mo>×</mml:mo><mml:msub><mml:mi>f</mml:mi><mml:mtext>flow</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>, is the total dilution factor, which arises from the low operating pressure of 200 <inline-formula><mml:math id="M351" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">mbar</mml:mi></mml:mrow></mml:math></inline-formula> and the additional small flow of humidified air containing a constant mixing ratio of <inline-formula><mml:math id="M352" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>. <inline-formula><mml:math id="M353" display="inline"><mml:mrow><mml:msub><mml:mi>f</mml:mi><mml:mtext>pressure</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> represents the pressure dilution factor given by the ratio of the ambient pressure to the operation pressure, equal to <inline-formula><mml:math id="M354" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 5. <inline-formula><mml:math id="M355" display="inline"><mml:mrow><mml:msub><mml:mi>f</mml:mi><mml:mtext>flow</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> is the flow dilution factor calculated as the ratio of the total flow rate of 6.25 <inline-formula><mml:math id="M356" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">L</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">min</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> to the sample flow rate of 6.0 <inline-formula><mml:math id="M357" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">L</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">min</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, equal to 1.04. Therefore, the total correction factor (<inline-formula><mml:math id="M358" display="inline"><mml:mi>f</mml:mi></mml:math></inline-formula>) is 5.2.</p>
      <p id="d2e5522">The instrument zero is critical for calculating <inline-formula><mml:math id="M359" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> from the observed OH decay rate and is usually assumed constant over a certain observation period. To evaluate instrument zero, OH decay rates were measured in zero air produced by a portable zero gas generator, yielding a <inline-formula><mml:math id="M360" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mtext>zero</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> of 5.2 <inline-formula><mml:math id="M361" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>. Several factors affect the instrument zero, including the self-reaction of OH, reaction of OH with <inline-formula><mml:math id="M362" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, OH diffusion, and reaction of OH with residual reactive species in zero air. The self-reaction rate constant of OH is 1.48 <inline-formula><mml:math id="M363" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<sup>−12</sup> <inline-formula><mml:math id="M365" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msup><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi mathvariant="normal">molec</mml:mi><mml:msup><mml:mo>.</mml:mo><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> at 298 <inline-formula><mml:math id="M366" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">K</mml:mi></mml:mrow></mml:math></inline-formula> (Atkinson et al., 2004), contributing to <inline-formula><mml:math id="M367" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 1.5 % of the instrument zero at the current OH concentration. The reaction rate constant of OH with <inline-formula><mml:math id="M368" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> is 7.3 <inline-formula><mml:math id="M369" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 10<sup>−14</sup> <inline-formula><mml:math id="M371" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msup><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi mathvariant="normal">molec</mml:mi><mml:msup><mml:mo>.</mml:mo><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> at 298 <inline-formula><mml:math id="M372" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">K</mml:mi></mml:mrow></mml:math></inline-formula> (Atkinson et al., 2004), leading to an OH loss rate of 0.3 <inline-formula><mml:math id="M373" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, which accounts for <inline-formula><mml:math id="M374" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 6 % of the instrument zero. The OH loss rate due to diffusion (<inline-formula><mml:math id="M375" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mtext>dif</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) under laminar flow conditions can be calculated from (Ivanov et al., 2007; Liu et al., 2009)
            <disp-formula id="Ch1.E10" content-type="numbered"><label>8</label><mml:math id="M376" display="block"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mtext>dif</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:msub><mml:mi>K</mml:mi><mml:mtext>dif</mml:mtext></mml:msub><mml:mo>×</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi>D</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow></mml:msub></mml:mrow><mml:mrow><mml:msubsup><mml:mi>r</mml:mi><mml:mtext>tube</mml:mtext><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where <inline-formula><mml:math id="M377" display="inline"><mml:mrow><mml:msub><mml:mi>K</mml:mi><mml:mtext>dif</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:mn mathvariant="normal">3.66</mml:mn></mml:mrow></mml:math></inline-formula> (for a cylinder cell) is the dimensionless geometric parameter, <inline-formula><mml:math id="M378" display="inline"><mml:mrow><mml:msub><mml:mi>r</mml:mi><mml:mtext>tube</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> is the radius of the cell, and <inline-formula><mml:math id="M379" display="inline"><mml:mrow><mml:msub><mml:mi>D</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M380" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 1.3 <inline-formula><mml:math id="M381" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> is the OH diffusion coefficient at 200 <inline-formula><mml:math id="M382" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">mbar</mml:mi></mml:mrow></mml:math></inline-formula> and 298 <inline-formula><mml:math id="M383" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">K</mml:mi></mml:mrow></mml:math></inline-formula> in air. The calculated OH diffusion loss rate was 0.8 <inline-formula><mml:math id="M384" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, giving a contribution of <inline-formula><mml:math id="M385" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 15 % of the instrument zero.</p>
      <p id="d2e5886">To assess the measurement precision of the LP-FRS instrument, an Allan deviation analysis was conducted on time series of zero-air measurements. The measured values were processed by subtracting the instrument zero. As shown in Fig. <xref ref-type="fig" rid="Ch1.F7"/>, the averaging time of the <inline-formula><mml:math id="M386" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> data point was 10 <inline-formula><mml:math id="M387" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">s</mml:mi></mml:mrow></mml:math></inline-formula>, with a total measurement time of about 4000 <inline-formula><mml:math id="M388" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">s</mml:mi></mml:mrow></mml:math></inline-formula>. The measurement precisions of <inline-formula><mml:math id="M389" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> were 2.3 and 1.7 <inline-formula><mml:math id="M390" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> with an acquisition time of 60 <inline-formula><mml:math id="M391" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">s</mml:mi></mml:mrow></mml:math></inline-formula> and 120 <inline-formula><mml:math id="M392" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">s</mml:mi></mml:mrow></mml:math></inline-formula>, respectively. When the averaging time increased to 300 <inline-formula><mml:math id="M393" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">s</mml:mi></mml:mrow></mml:math></inline-formula>, the atmospheric <inline-formula><mml:math id="M394" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> measurement precision could be further improved to 1.0 <inline-formula><mml:math id="M395" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>.</p>

      <fig id="Ch1.F7"><label>Figure 7</label><caption><p id="d2e6005"><bold>(a)</bold> Time series of zero air with 10 <inline-formula><mml:math id="M396" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">s</mml:mi></mml:mrow></mml:math></inline-formula> time resolution and <bold>(b)</bold> the Allan deviation analysis of the time series. The measurement precision of <inline-formula><mml:math id="M397" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> can be improved to 2.3 and 1.0 <inline-formula><mml:math id="M398" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> with averaging times of 60 <inline-formula><mml:math id="M399" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">s</mml:mi></mml:mrow></mml:math></inline-formula> and 300 <inline-formula><mml:math id="M400" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">s</mml:mi></mml:mrow></mml:math></inline-formula>, respectively.</p></caption>
          <graphic xlink:href="https://amt.copernicus.org/articles/18/1243/2025/amt-18-1243-2025-f07.png"/>

        </fig>

      <p id="d2e6072">A comprehensive approach to evaluating the instrument's total uncertainty is measuring zero air. Figure <xref ref-type="fig" rid="Ch1.F8"/> illustrates the <inline-formula><mml:math id="M401" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> values obtained from zero air on different days. Each value was obtained from 1 h continuous measurements. The time intervals for these zero-value measurements are longer than 2 weeks. The error bars of the data points agreed well with the <inline-formula><mml:math id="M402" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> measurement precision obtained from Allan deviation analysis. No significant drift was found during measurements, with a mean value close to zero at 0.2 <inline-formula><mml:math id="M403" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>. The <inline-formula><mml:math id="M404" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> measurement uncertainty of the developed LP-FRS instrument, which can be determined from the deviations of these measurements, was within 2 <inline-formula><mml:math id="M405" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>. The uncertainty of the LP-FRS instrument arises from two main sources: the dilution factor and the instrument zero. The uncertainties associated with the mass flowmeters and the pressure controller used were <inline-formula><mml:math id="M406" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 1 % and <inline-formula><mml:math id="M407" display="inline"><mml:mo>&lt;</mml:mo></mml:math></inline-formula> 1 %, respectively, resulting in a total uncertainty of the dilution correction factor of less than 2 %. The uncertainty of the instrument zero primarily originates from various influencing factors, such as changes in <inline-formula><mml:math id="M408" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> concentrations and residual reactants in zero air and water.</p>

      <fig id="Ch1.F8"><label>Figure 8</label><caption><p id="d2e6175">Measured <inline-formula><mml:math id="M409" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> values of zero air on different days. The total instrument uncertainty, determined from the measurement deviations, is within 2 <inline-formula><mml:math id="M410" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>.</p></caption>
          <graphic xlink:href="https://amt.copernicus.org/articles/18/1243/2025/amt-18-1243-2025-f08.png"/>

        </fig>

</sec>
</sec>
<sec id="Ch1.S4">
  <label>4</label><title>Field performance</title>
      <p id="d2e6221">The capability of the developed LP-FRS instrument was demonstrated through field measurements of atmospheric total OH reactivity. Measurements were conducted at the park of the Hefei Institutes of Physical Science, Chinese Academy of Sciences (31°91<sup>′</sup> N, 117°16<sup>′</sup> E) (Khayyam et al., 2024). This observation site is situated on a peninsula in a suburban area, surrounded by water on three sides. There were also an optical factory and several mechanical processing factories located on the peninsula. The observation period spanned 1 to 4 May 2023.</p>
      <p id="d2e6242">The LP-FRS instrument was housed in a container with the sampling port positioned <inline-formula><mml:math id="M413" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 1.2 <inline-formula><mml:math id="M414" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi></mml:mrow></mml:math></inline-formula> above the container's roof. In addition to measuring OH reactivity, concentrations of 115 kinds of VOCs were analysed using a gas chromatograph coupled with a flame ionization detector and mass spectrometer (GC-FID/MS; TSQ 9000, Thermo Fisher) with a time resolution of 1 <inline-formula><mml:math id="M415" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">h</mml:mi></mml:mrow></mml:math></inline-formula>. The VOCs included 29 alkanes (alka), 12 alkenes (alke), 16 aromatic hydrocarbons (arom), 35 halogenated hydrocarbons (halo), 21 oxygenated volatile organic compounds (OVOCs), 1 alkyne, and 1 carbon disulfide. Concentrations of NO, <inline-formula><mml:math id="M416" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, and <inline-formula><mml:math id="M417" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> were measured employing an <inline-formula><mml:math id="M418" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mi>x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> analyser (42i, Thermo Fisher) and an <inline-formula><mml:math id="M419" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> analyser (49i, Thermo Fisher). Data of ambient temperature (<inline-formula><mml:math id="M420" display="inline"><mml:mi>T</mml:mi></mml:math></inline-formula>) and relative humidity (RH) were obtained from an automatic monitoring station located <inline-formula><mml:math id="M421" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 100 <inline-formula><mml:math id="M422" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi></mml:mrow></mml:math></inline-formula> from the container. The photolysis rate constant of <inline-formula><mml:math id="M423" display="inline"><mml:mrow><mml:mi>J</mml:mi><mml:mo>(</mml:mo><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula> was measured with a photolysis spectrometer (PFS-100, Focused Photonics).</p>

      <fig id="Ch1.F9" specific-use="star"><label>Figure 9</label><caption><p id="d2e6355">Time series of observed meteorological and chemical parameters, including ambient temperature; relative humidity; total OH reactivity; photolysis frequencies (<inline-formula><mml:math id="M424" display="inline"><mml:mrow><mml:mi>J</mml:mi><mml:mo>(</mml:mo><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula>); and concentrations of <inline-formula><mml:math id="M425" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, NO, <inline-formula><mml:math id="M426" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, and VOCs. The time period is from 1 to 4 May 2023.</p></caption>
        <graphic xlink:href="https://amt.copernicus.org/articles/18/1243/2025/amt-18-1243-2025-f09.png"/>

      </fig>

      <fig id="Ch1.F10"><label>Figure 10</label><caption><p id="d2e6407"><bold>(a)</bold> Stack of diurnal profiles of observed <inline-formula><mml:math id="M427" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> compared with calculated OH reactivity from individual groups of measured atmospheric species; <bold>(b)</bold> pie chart of contributions from each group to total reactivity.</p></caption>
        <graphic xlink:href="https://amt.copernicus.org/articles/18/1243/2025/amt-18-1243-2025-f10.png"/>

      </fig>

      <p id="d2e6435">An overview of observed meteorological and gas concentrations is given in Fig. <xref ref-type="fig" rid="Ch1.F9"/>. The average temperature and relative humidity during the observation period were 25.6 <inline-formula><mml:math id="M428" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">°</mml:mi><mml:mi mathvariant="normal">C</mml:mi></mml:mrow></mml:math></inline-formula> (range from 21.9 to 30.8 <inline-formula><mml:math id="M429" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">°</mml:mi><mml:mi mathvariant="normal">C</mml:mi></mml:mrow></mml:math></inline-formula>) and 53.8 % (range from 21 % to 90 %), respectively. The large changes in <inline-formula><mml:math id="M430" display="inline"><mml:mrow><mml:mi>J</mml:mi><mml:mo>(</mml:mo><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula> were due to the rainy weather on 3 May and cloudy conditions on 4 May. Table <xref ref-type="table" rid="Ch1.T2"/> summarizes the mean and median concentrations of the measured species during the observation period. The mean concentrations of NO, <inline-formula><mml:math id="M431" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, and <inline-formula><mml:math id="M432" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> were 1.5, 10.0, and 36.7 <inline-formula><mml:math id="M433" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">ppbv</mml:mi></mml:mrow></mml:math></inline-formula>, respectively. Alkanes, OVOCs, and hydrocarbons were the three VOCs with the highest concentrations during the period. The corresponding mean concentrations were 9.1, 7.1, and 4.9 <inline-formula><mml:math id="M434" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">ppbv</mml:mi></mml:mrow></mml:math></inline-formula>, respectively. The measured BVOCs only include isoprene, with a mean concentration of 0.2 <inline-formula><mml:math id="M435" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">ppbv</mml:mi></mml:mrow></mml:math></inline-formula>. The minimum and maximum values of <inline-formula><mml:math id="M436" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> were 10.6 and 30.0 <inline-formula><mml:math id="M437" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, respectively.</p>

<table-wrap id="Ch1.T2"><label>Table 2</label><caption><p id="d2e6559">The mean and median concentrations of measured species during the observation period in the form of classification.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="3">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="right"/>
     <oasis:colspec colnum="3" colname="col3" align="right"/>
     <oasis:thead>
       <oasis:row>
         <oasis:entry colname="col1">Measured species</oasis:entry>
         <oasis:entry colname="col2">Average</oasis:entry>
         <oasis:entry colname="col3">Median</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2">concentrations</oasis:entry>
         <oasis:entry colname="col3">concentrations</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2">(<inline-formula><mml:math id="M438" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">ppbv</mml:mi></mml:mrow></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col3">(<inline-formula><mml:math id="M439" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">ppbv</mml:mi></mml:mrow></mml:math></inline-formula>)</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>
         <oasis:entry colname="col1">NO</oasis:entry>
         <oasis:entry colname="col2">1.5</oasis:entry>
         <oasis:entry colname="col3">0.3</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"><inline-formula><mml:math id="M440" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2">10.0</oasis:entry>
         <oasis:entry colname="col3">8.9</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"><inline-formula><mml:math id="M441" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2">36.7</oasis:entry>
         <oasis:entry colname="col3">36.9</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">Alka</oasis:entry>
         <oasis:entry colname="col2">9.1</oasis:entry>
         <oasis:entry colname="col3">9.0</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">Alke</oasis:entry>
         <oasis:entry colname="col2">3.8</oasis:entry>
         <oasis:entry colname="col3">3.1</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">Arom</oasis:entry>
         <oasis:entry colname="col2">2.3</oasis:entry>
         <oasis:entry colname="col3">2.2</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">Halo</oasis:entry>
         <oasis:entry colname="col2">4.9</oasis:entry>
         <oasis:entry colname="col3">4.6</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">BVOCs (including</oasis:entry>
         <oasis:entry colname="col2">0.2</oasis:entry>
         <oasis:entry colname="col3">0.1</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">only isoprene)</oasis:entry>
         <oasis:entry colname="col2"/>
         <oasis:entry colname="col3"/>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">OVOCs</oasis:entry>
         <oasis:entry colname="col2">7.1</oasis:entry>
         <oasis:entry colname="col3">7.1</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table></table-wrap>

      <p id="d2e6766">The reactive species and <inline-formula><mml:math id="M442" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> exhibited distinct daily variations on 1 May (the first day of the International Labour Day holiday). The peak of VOC concentrations (60 <inline-formula><mml:math id="M443" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">ppbv</mml:mi></mml:mrow></mml:math></inline-formula>) appeared at 03:00 LT. The concentrations of NO began increasing significantly from 03:00 LT onwards, reaching a peak of 23.7 <inline-formula><mml:math id="M444" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">ppbv</mml:mi></mml:mrow></mml:math></inline-formula> around 05:00 LT. Concurrently, the abundant NO reacted with <inline-formula><mml:math id="M445" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, resulting in the lowest observed <inline-formula><mml:math id="M446" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> concentration (<inline-formula><mml:math id="M447" display="inline"><mml:mo lspace="0mm">∼</mml:mo></mml:math></inline-formula> 5 <inline-formula><mml:math id="M448" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">ppbv</mml:mi></mml:mrow></mml:math></inline-formula>) and an increase in <inline-formula><mml:math id="M449" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> level. <inline-formula><mml:math id="M450" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M451" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> reached their peak values of 30.0 <inline-formula><mml:math id="M452" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> and 29.3 <inline-formula><mml:math id="M453" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">ppbv</mml:mi></mml:mrow></mml:math></inline-formula> at about 08:00 LT in the morning, declining rapidly as sunlight intensified, with the lowest values observed between 12:00 and 13:00 LT. The highest <inline-formula><mml:math id="M454" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> concentration (59.3 <inline-formula><mml:math id="M455" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">ppbv</mml:mi></mml:mrow></mml:math></inline-formula>) occurred around 17:00 LT in the afternoon. <inline-formula><mml:math id="M456" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> and reactive species exhibited relatively low values in the following days, and no significant peak in NO concentration was observed in the afternoon. These changes could be attributed to the “holiday effect” (Fatahi et al., 2021), which reflects extensive vehicle travel on the eve and the first day of the holiday and decreased human activities near the observation site during the holiday (Song et al., 2022).</p>
      <p id="d2e6929">A zero-dimensional box model (Framework for 0-Dimensional Atmospheric Modelling, F0AM) based on the Master Chemical Mechanism (MCM3.3.1, <uri>https://mcm.york.ac.uk/MCM/</uri>, last access: 30 July 2024) was applied for comparison with the observed total OH reactivity (Wolfe et al., 2016; Wei et al., 2023). The model was constrained by the measured species and parameters of meteorology and photolysis. Figure <xref ref-type="fig" rid="Ch1.F10"/>a shows the diurnal profiles of observed and simulated <inline-formula><mml:math id="M457" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula>. The observed <inline-formula><mml:math id="M458" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> ranged from 14.6 <inline-formula><mml:math id="M459" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> (at 14:00 LT) to 21.9 <inline-formula><mml:math id="M460" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> (at 08:00 LT), with an average value of 17.5 <inline-formula><mml:math id="M461" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>. According to the pie chart analysis in Fig. <xref ref-type="fig" rid="Ch1.F10"/>b, inorganic species, alkenes, OVOCs, and alkanes contributed 26.4 %, 10.8 %, 10.5 %, and 5.0 % to the <inline-formula><mml:math id="M462" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula>, respectively. Contributions from aromatic and halogenated hydrocarbons were relatively low, accounting for 3.0 % and 0.6 %. The contribution of photochemical secondary products (others) was as high as 20.9 %, while the missing reactivity (i.e. the difference between observed and simulated <inline-formula><mml:math id="M463" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula> averaged <inline-formula><mml:math id="M464" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 20.5 %, highlighting the significant role of photochemical and unidentified components in local atmospheric chemistry.</p>
</sec>
<sec id="Ch1.S5" sec-type="conclusions">
  <label>5</label><title>Conclusions</title>
      <p id="d2e7056">A portable LP-FRS instrument was developed. A specific Herriott-type pump–probe MPC with a small multi-pass beam distribution circle radius of 3.7 <inline-formula><mml:math id="M465" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">mm</mml:mi></mml:mrow></mml:math></inline-formula> at the centre of the cell was designed to offer an effective overlapping path length of <inline-formula><mml:math id="M466" display="inline"><mml:mo>∼</mml:mo></mml:math></inline-formula> 28.5 <inline-formula><mml:math id="M467" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">m</mml:mi></mml:mrow></mml:math></inline-formula> between the mid-infrared probe light and the photolysis light with a high overlapping factor of 75.4 %. Such an overlapping factor benefits from reducing instrument size, resulting in dimensions of just 130 <inline-formula><mml:math id="M468" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M469" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 40 <inline-formula><mml:math id="M470" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M471" display="inline"><mml:mo>×</mml:mo></mml:math></inline-formula> 35 <inline-formula><mml:math id="M472" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">cm</mml:mi></mml:mrow></mml:math></inline-formula>. The precision and uncertainty of the LP-FRS instrument for measuring atmospheric <inline-formula><mml:math id="M473" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> were 1.0 <inline-formula><mml:math id="M474" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> (1<inline-formula><mml:math id="M475" display="inline"><mml:mi mathvariant="italic">σ</mml:mi></mml:math></inline-formula>, 300 <inline-formula><mml:math id="M476" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">s</mml:mi></mml:mrow></mml:math></inline-formula>) and within 2 <inline-formula><mml:math id="M477" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula>, respectively. A field test was performed at a suburban site, where the averaged measured <inline-formula><mml:math id="M478" display="inline"><mml:mrow><mml:msubsup><mml:mi>k</mml:mi><mml:mrow class="chem"><mml:mi mathvariant="normal">OH</mml:mi></mml:mrow><mml:mo>′</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula> was 17.5 <inline-formula><mml:math id="M479" display="inline"><mml:mrow class="unit"><mml:msup><mml:mi mathvariant="normal">s</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> with a missing reactivity of 20.5 % compared to the model-simulated result based on measured species. The developed portable LP-FRS instrument expands the measurement capabilities for atmospheric total OH reactivity and will be employed in more field observations.</p>
</sec>

      
      </body>
    <back><notes notes-type="dataavailability"><title>Data availability</title>

      <p id="d2e7211">The data used in this study can be obtained from the Science Data Bank accessible at <ext-link xlink:href="https://doi.org/10.57760/sciencedb.19568" ext-link-type="DOI">10.57760/sciencedb.19568</ext-link> (Fang et al., 2025).</p>
  </notes><notes notes-type="authorcontribution"><title>Author contributions</title>

      <p id="d2e7220">BF and WZhao designed the research. BF, WZhao, and NY built the instrument. BF, JL, and HeZ conducted the instrument test. BF and HaZ analysed the data. NW performed the simulation. BF and WZhang wrote the paper. YaL, ZZ, and YuL helped during the field test. All authors discussed the results and commented on the paper.</p>
  </notes><notes notes-type="competinginterests"><title>Competing interests</title>

      <p id="d2e7226">The contact author has declared that none of the authors has any competing interests.</p>
  </notes><notes notes-type="disclaimer"><title>Disclaimer</title>

      <p id="d2e7232">Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors.</p>
  </notes><notes notes-type="financialsupport"><title>Financial support</title>

      <p id="d2e7238">This research has been supported by the National Key Research and Development Program of China (grant nos. 2022YFC3700304, 2023YFC3705502), the National Natural Science Foundation of China (grant nos. U21A2028, 42105099, 91544228), the 2024 industrialization fund of Wanjiang Emerging Industry Technology Development Centre (grant no. WJ24CYHXM03), and the HFIPS Director's Fund (grant nos. BJPY2023A02, YZJJ202101).</p>
  </notes><notes notes-type="reviewstatement"><title>Review statement</title>

      <p id="d2e7244">This paper was edited by Anna Novelli and reviewed by three anonymous referees.</p>
  </notes><ref-list>
    <title>References</title>

      <ref id="bib1.bib1"><label>1</label><mixed-citation>Atkinson, R., Baulch, D. L., Cox, R. A., Crowley, J. N., Hampson, R. F., Hynes, R. G., Jenkin, M. E., Rossi, M. J., and Troe, J.: Evaluated kinetic and photochemical data for atmospheric chemistry: Volume I – gas phase reactions of <inline-formula><mml:math id="M480" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mi mathvariant="normal">x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M481" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">HO</mml:mi><mml:mi mathvariant="normal">x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M482" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mi mathvariant="normal">x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M483" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">SO</mml:mi><mml:mi mathvariant="normal">x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> species, Atmos. Chem. Phys., 4, 1461–1738, <ext-link xlink:href="https://doi.org/10.5194/acp-4-1461-2004" ext-link-type="DOI">10.5194/acp-4-1461-2004</ext-link>, 2004.</mixed-citation></ref>
      <ref id="bib1.bib2"><label>2</label><mixed-citation>Atkinson, R., Baulch, D. L., Cox, R. A., Crowley, J. N., Hampson, R. F., Hynes, R. G., Jenkin, M. E., Rossi, M. J., Troe, J., and IUPAC Subcommittee: Evaluated kinetic and photochemical data for atmospheric chemistry: Volume II – gas phase reactions of organic species, Atmos. Chem. Phys., 6, 3625–4055, <ext-link xlink:href="https://doi.org/10.5194/acp-6-3625-2006" ext-link-type="DOI">10.5194/acp-6-3625-2006</ext-link>, 2006.</mixed-citation></ref>
      <ref id="bib1.bib3"><label>3</label><mixed-citation>Brecha, R. J., Pedrotti, L. M., and Krause, D.: Magnetic rotation spectroscopy of molecular oxygen with a diode laser, J. Opt. Soc. Am. B, 14, 1921–1930, <ext-link xlink:href="https://doi.org/10.1063/1.1149176" ext-link-type="DOI">10.1063/1.1149176</ext-link>, 1997.</mixed-citation></ref>
      <ref id="bib1.bib4"><label>4</label><mixed-citation>Cheng, F., Zhao, W., Fang, B., Zhang, Y., Yang, N., Zhou, H., and Zhang, W.: High band-width mid-infrared frequency-modulated Faraday rotation spectrometer for time resolved measurement of the OH radical, Opt. Express, 31, 25058–25069, <ext-link xlink:href="https://doi.org/10.1364/OE.493270" ext-link-type="DOI">10.1364/OE.493270</ext-link>, 2023.</mixed-citation></ref>
      <ref id="bib1.bib5"><label>5</label><mixed-citation>Di Carlo, P., Brune, W. H., Martinez, M., Harder, H., Lesher, R., Ren, X., Thornberry, T., Carroll, M. A., Young, V., Shepson, P. B., Riemer, D., Apel, E., and Campbell, C.: Missing OH reactivity in a forest: evidence for unknown reactive biogenic VOCs, Science, 304, 722–725, <ext-link xlink:href="https://doi.org/10.1126/science.1094392" ext-link-type="DOI">10.1126/science.1094392</ext-link>, 2004.</mixed-citation></ref>
      <ref id="bib1.bib6"><label>6</label><mixed-citation>Fang, B., Yang, N., Wang, C., Zhao, W., Xu, X., Zhang, Y., and Zhang, W.: Detection of nitric oxide with Faraday rotation spectroscopy at 5.33 <inline-formula><mml:math id="M484" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi><mml:mi mathvariant="normal">m</mml:mi></mml:mrow></mml:math></inline-formula>, Chin. J. Chem. Phys., 33, 37–42, <ext-link xlink:href="https://doi.org/10.1063/1674-0068/cjcp1910182" ext-link-type="DOI">10.1063/1674-0068/cjcp1910182</ext-link>, 2020.</mixed-citation></ref>
      <ref id="bib1.bib7"><label>7</label><mixed-citation>Fang, B., Wei, N., Zhao, W., Yang, N., Zhou, H., Zhang, H., Li, J., Zhang, W., Lu, Y., Zhu, Z., and Liu, Y.: Data used in preprint of “Development of a portable laser-flash photolysis Faraday rotation spectrometer for measuring atmospheric total OH reactivity” [DS/OL], V1, Science Data Bank [data set], <ext-link xlink:href="https://doi.org/10.57760/sciencedb.19568" ext-link-type="DOI">10.57760/sciencedb.19568</ext-link>, 2025.</mixed-citation></ref>
      <ref id="bib1.bib8"><label>8</label><mixed-citation>Fatahi, Y., Kouznetsov, R., and Sofiev, M.: The effect of accounting for public holidays on the skills of the atmospheric composition model SILAM v.5.7, Geosci. Model Dev., 14, 7459–7475, <ext-link xlink:href="https://doi.org/10.5194/gmd-14-7459-2021" ext-link-type="DOI">10.5194/gmd-14-7459-2021</ext-link>, 2021.</mixed-citation></ref>
      <ref id="bib1.bib9"><label>9</label><mixed-citation>Fuchs, H., Hofzumahaus, A., Rohrer, F., Bohn, B., Brauers, T., Dorn, H. P., Häseler, R., Holland, F., Kaminski, M., Li, X., Lu, K., Nehr, S., Tillmann, R., Wegener, R., and Wahner, A.: Experimental evidence for efficient hydroxyl radical regeneration in isoprene oxidation, Nat. Geosci., 6, 1023–1026, <ext-link xlink:href="https://doi.org/10.1038/ngeo1964" ext-link-type="DOI">10.1038/ngeo1964</ext-link>, 2013.</mixed-citation></ref>
      <ref id="bib1.bib10"><label>10</label><mixed-citation>Fuchs, H., Novelli, A., Rolletter, M., Hofzumahaus, A., Pfannerstill, E. Y., Kessel, S., Edtbauer, A., Williams, J., Michoud, V., Dusanter, S., Locoge, N., Zannoni, N., Gros, V., Truong, F., Sarda-Esteve, R., Cryer, D. R., Brumby, C. A., Whalley, L. K., Stone, D., Seakins, P. W., Heard, D. E., Schoemaecker, C., Blocquet, M., Coudert, S., Batut, S., Fittschen, C., Thames, A. B., Brune, W. H., Ernest, C., Harder, H., Muller, J. B. A., Elste, T., Kubistin, D., Andres, S., Bohn, B., Hohaus, T., Holland, F., Li, X., Rohrer, F., Kiendler-Scharr, A., Tillmann, R., Wegener, R., Yu, Z., Zou, Q., and Wahner, A.: Comparison of OH reactivity measurements in the atmospheric simulation chamber SAPHIR, Atmos. Meas. Tech., 10, 4023–4053, <ext-link xlink:href="https://doi.org/10.5194/amt-10-4023-2017" ext-link-type="DOI">10.5194/amt-10-4023-2017</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib11"><label>11</label><mixed-citation>Goldstein, A. H. and Galbally, I. E.: Known and unexplored organic constituents in the Earth's atmosphere, Environ. Sci. Technol., 41, 1514–1521, <ext-link xlink:href="https://doi.org/10.1021/es072476p" ext-link-type="DOI">10.1021/es072476p</ext-link>, 2007.</mixed-citation></ref>
      <ref id="bib1.bib12"><label>12</label><mixed-citation>Gordon, I. E., Rothman, L. S., Hargreaves, R. J., Hashemi, R., Karlovets, E. V., Skinner, F. M., Conway, E. K., Hill, C., Kochanov, R. V., Tan, Y., Wcisło, P., Finenko, A. A., Nelson, K., Bernath, P. F., Birk, M., Boudon, V., Campargue, A., Chance, K. V., Coustenis, A., Drouin, B. J., Flaud, J. M., Gamache, R. R., Hodges, J. T., Jacquemart, D., Mlawer, E. J., Nikitin, A. V., Perevalov, V. I., Rotger, M., Tennyson, J., Toon, G. C., Tran, H., Tyuterev, V. G., Adkins, E. M., Baker, A., Barbe, A., Canè, E., Császár, A. G., Dudaryonok, A., Egorov, O., Fleisher, A. J., Fleurbaey, H., Foltynowicz, A., Furtenbacher, T., Harrison, J. J., Hartmann, J. M., Horneman, V. M., Huang, X., Karman, T., Karns, J., Kassi, S., Kleiner, I., Kofman, V., Kwabia-Tchana, F., Lavrentieva, N. N., Lee, T. J., Long, D. A., Lukashevskaya, A. A., Lyulin, O. M., Makhnev, V. Y., Matt, W., Massie, S. T., Melosso, M., Mikhailenko, S. N., Mondelain, D., Müller, H. S. P., Naumenko, O. V., Perrin, A., Polyansky, O. L., Raddaoui, E., Raston, P. L., Reed, Z. D., Rey, M., Richard, C., Tóbiás, R., Sadiek, I., Schwenke, D. W., Starikova, E., Sung, K., Tamassia, F., Tashkun, S. A., Auwera, J. V., Vasilenko, I. A., Vigasin, A. A., Villanueva, G. L., Vispoel, B., Wagner, G., Yachmenev, A., and Yurchenko, S. N.: The HITRAN2020 molecular spectroscopic database, J. Quant. Spectrosc. Ra., 277, 107949, <ext-link xlink:href="https://doi.org/10.1016/j.jqsrt.2021.107949" ext-link-type="DOI">10.1016/j.jqsrt.2021.107949</ext-link>, 2022.</mixed-citation></ref>
      <ref id="bib1.bib13"><label>13</label><mixed-citation>Hansen, R. F., Griffith, S. M., Dusanter, S., Rickly, P. S., Stevens, P. S., Bertman, S. B., Carroll, M. A., Erickson, M. H., Flynn, J. H., Grossberg, N., Jobson, B. T., Lefer, B. L., and Wallace, H. W.: Measurements of total hydroxyl radical reactivity during CABINEX 2009 – Part 1: field measurements, Atmos. Chem. Phys., 14, 2923–2937, <ext-link xlink:href="https://doi.org/10.5194/acp-14-2923-2014" ext-link-type="DOI">10.5194/acp-14-2923-2014</ext-link>, 2014.</mixed-citation></ref>
      <ref id="bib1.bib14"><label>14</label><mixed-citation>Hansen, R. F., Blocquet, M., Schoemaecker, C., Léonardis, T., Locoge, N., Fittschen, C., Hanoune, B., Stevens, P. S., Sinha, V., and Dusanter, S.: Intercomparison of the comparative reactivity method (CRM) and pump–probe technique for measuring total OH reactivity in an urban environment, Atmos. Meas. Tech., 8, 4243–4264, <ext-link xlink:href="https://doi.org/10.5194/amt-8-4243-2015" ext-link-type="DOI">10.5194/amt-8-4243-2015</ext-link>, 2015.</mixed-citation></ref>
      <ref id="bib1.bib15"><label>15</label><mixed-citation>Heald, C. L., de Gouw, J., Goldstein, A. H., Guenther, A. B., Hayes, P. L., Hu, W., Isaacman-VanWertz, G., Jimenez, J. L., Keutsch, F. N., Koss, A. R., Misztal, P. K., Rappenglück, B., Roberts, J. M., Stevens, P. S., Washenfelder, R. A., Warneke, C., and Young, C. J.: Contrasting reactive organic carbon observations in the southeast United States (SOAS) and southern California (CalNex), Environ. Sci. Technol., 54, 14923–14935, <ext-link xlink:href="https://doi.org/10.1021/acs.est.0c05027" ext-link-type="DOI">10.1021/acs.est.0c05027</ext-link>, 2020.</mixed-citation></ref>
      <ref id="bib1.bib16"><label>16</label><mixed-citation>Hens, K., Novelli, A., Martinez, M., Auld, J., Axinte, R., Bohn, B., Fischer, H., Keronen, P., Kubistin, D., Nölscher, A. C., Oswald, R., Paasonen, P., Petäjä, T., Regelin, E., Sander, R., Sinha, V., Sipilä, M., Taraborrelli, D., Tatum Ernest, C., Williams, J., Lelieveld, J., and Harder, H.: Observation and modelling of <inline-formula><mml:math id="M485" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">HO</mml:mi><mml:mi mathvariant="normal">x</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> radicals in a boreal forest, Atmos. Chem. Phys., 14, 8723–8747, <ext-link xlink:href="https://doi.org/10.5194/acp-14-8723-2014" ext-link-type="DOI">10.5194/acp-14-8723-2014</ext-link>, 2014.</mixed-citation></ref>
      <ref id="bib1.bib17"><label>17</label><mixed-citation>Hunter, J. F., Day, D. A., Palm, B. B., Yatavelli, R. L. N., Chan, A. W. H., Kaser, L., Cappellin, L., Hayes, P. L., Cross, E. S., Carrasquillo, A. J., Campuzano-Jost, P., Stark, H., Zhao, Y., Hohaus, T., Smith, J. N., Hansel, A., Karl, T., Goldstein, A. H., Guenther, A., Worsnop, D. R., Thornton, J. A., Heald, C. L., Jimenez, J. L., and Kroll, J. H.: Comprehensive characterization of atmospheric organic carbon at a forested site, Nat. Geosci., 10, 748–753, <ext-link xlink:href="https://doi.org/10.1038/NGEO3018" ext-link-type="DOI">10.1038/NGEO3018</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib18"><label>18</label><mixed-citation>Ingham, T., Goddard, A., Whalley, L. K., Furneaux, K. L., Edwards, P. M., Seal, C. P., Self, D. E., Johnson, G. P., Read, K. A., Lee, J. D., and Heard, D. E.: A flow-tube based laser-induced fluorescence instrument to measure OH reactivity in the troposphere, Atmos. Meas. Tech., 2, 465–477, <ext-link xlink:href="https://doi.org/10.5194/amt-2-465-2009" ext-link-type="DOI">10.5194/amt-2-465-2009</ext-link>, 2009.</mixed-citation></ref>
      <ref id="bib1.bib19"><label>19</label><mixed-citation>Ivanov, A. V., Trakhtenberg, S., Bertram, A. K., Gershenzon, Y. M., and Molina, M. J.: OH, <inline-formula><mml:math id="M486" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">HO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, and ozone gaseous diffusion coefficients, J. Phys. Chem. A, 111, 1632–1637, <ext-link xlink:href="https://doi.org/10.1021/jp066558w" ext-link-type="DOI">10.1021/jp066558w</ext-link>, 2007.</mixed-citation></ref>
      <ref id="bib1.bib20"><label>20</label><mixed-citation>Khayyam, J., Xie, P., Xu, J., Tian, X., Feng, H., and Qinjin, W.: Vertically resolved meteorological adjustments of aerosols and trace gases in Beijing, Taiyuan, and Hefei by using RF model, Sci. Total Environ., 948, 174795, <ext-link xlink:href="https://doi.org/10.1016/j.scitotenv.2024.174795" ext-link-type="DOI">10.1016/j.scitotenv.2024.174795</ext-link>, 2024.</mixed-citation></ref>
      <ref id="bib1.bib21"><label>21</label><mixed-citation>Kim, S., Sanchez, D., Wang, M., Seco, R., Jeong, D., Hughes, S., Barletta, B., Blake, D. R., Jung, J., Kim, D., Lee, G., Lee, M., Ahn, J., Lee, S.-D., Cho, G., Sung, M. Y., Lee, Y. H., Kim, D. B., Kim, Y., Woo, J. H., Jo, D., Park, R., Park, J. H., Hong, Y. D., and Hong, J. H.: OH reactivity in urban and suburban regions in Seoul, South Korea – an East Asian megacity in a rapid transition, Faraday Discuss., 189, 231–251, <ext-link xlink:href="https://doi.org/10.1039/C5FD00230C" ext-link-type="DOI">10.1039/C5FD00230C</ext-link>, 2016.</mixed-citation></ref>
      <ref id="bib1.bib22"><label>22</label><mixed-citation>Kohno, N., Zhou, J., Li, J., Takemura, M., Ono, N., Sadanaga, Y., Nakashima, Y., Sato, K., Kato, S., Sakamoto, Y., and Kajii, Y.: Impacts of missing OH reactivity and aerosol uptake of <inline-formula><mml:math id="M487" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">HO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> radicals on tropospheric <inline-formula><mml:math id="M488" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> production during the AQUAS-Kyoto summer campaign in 2018, Atmos. Environ., 281, 119130, <ext-link xlink:href="https://doi.org/10.1016/j.atmosenv.2022.119130" ext-link-type="DOI">10.1016/j.atmosenv.2022.119130</ext-link>, 2022.</mixed-citation></ref>
      <ref id="bib1.bib23"><label>23</label><mixed-citation>Kovacs, T. A. and Brune, W. H.: Total OH loss rate measurement, J. Atmos. Chem., 39, 105–122, <ext-link xlink:href="https://doi.org/10.1023/A:1010614113786" ext-link-type="DOI">10.1023/A:1010614113786</ext-link>, 2001.</mixed-citation></ref>
      <ref id="bib1.bib24"><label>24</label><mixed-citation>Kumar, V. and Sinha, V.: VOC-OHM: A new technique for rapid measurements of ambient total OH reactivity and volatile organic compounds using a single proton transfer reaction mass spectrometer, Int. J. Mass Spectrom., 374, 55–63, <ext-link xlink:href="https://doi.org/10.1016/j.ijms.2014.10.012" ext-link-type="DOI">10.1016/j.ijms.2014.10.012</ext-link>, 2014.</mixed-citation></ref>
      <ref id="bib1.bib25"><label>25</label><mixed-citation>Lawrence, M. G.: The relationship between relative humidity and the dewpoint temperature in moist air, B. Am. Meteorol. Soc., 86, 225–234, <ext-link xlink:href="https://doi.org/10.1175/BAMS-86-2-225" ext-link-type="DOI">10.1175/BAMS-86-2-225</ext-link>, 2005.</mixed-citation></ref>
      <ref id="bib1.bib26"><label>26</label><mixed-citation>Lewicki, R., Doty III, J. H., Curl, R. F., Tittel, F. K., and Wysocki, G.: Ultrasensitive detection of nitric oxide at 5.33 <inline-formula><mml:math id="M489" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi><mml:mi mathvariant="normal">m</mml:mi></mml:mrow></mml:math></inline-formula> by using external cavity quantum cascade laser-based Faraday rotation spectroscopy, P. Natl. Acad. Sci. USA, 106, 12587–12592, <ext-link xlink:href="https://doi.org/10.1073/pnas.0906291106" ext-link-type="DOI">10.1073/pnas.0906291106</ext-link>, 2009.</mixed-citation></ref>
      <ref id="bib1.bib27"><label>27</label><mixed-citation>Lewis, T., Heard, D. E., and Blitz, M. A.: A novel multiplex absorption spectrometer for time-resolved studies, Rev. Sci. Instrum., 89, 024101, <ext-link xlink:href="https://doi.org/10.1063/1.5006539" ext-link-type="DOI">10.1063/1.5006539</ext-link>, 2018.</mixed-citation></ref>
      <ref id="bib1.bib28"><label>28</label><mixed-citation>Li, J., Kohno, N., Sakamoto, Y., Fukusaki, Y., Kousa, Y., Sadanaga, Y., Nakashima, Y., Sato, K., Ramasamy, S., Takami, A., Yoshino, A., Nakayama, T., Kato, S., Ono, N., Zhou, J., Bai, Y., and Kajii, Y.: A quantitative understanding of total OH reactivity and ozone production in a coastal industrial area during the Yokohama air quality study (AQUAS) campaign of summer 2019, Atmos. Environ., 267, 118754, <ext-link xlink:href="https://doi.org/10.1016/j.atmosenv.2021.118754" ext-link-type="DOI">10.1016/j.atmosenv.2021.118754</ext-link>, 2021.</mixed-citation></ref>
      <ref id="bib1.bib29"><label>29</label><mixed-citation>Li, J., Kohno, N., Sakamoto, Y., Pham, H. G., Murano, K., Sato, K., Nakayama, T., and Kajii, Y.: Potential factors contributing to ozone production in AQUAS-Kyoto campaign in summer 2020: natural source-related missing OH reactivity and heterogeneous <inline-formula><mml:math id="M490" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">HO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>/<inline-formula><mml:math id="M491" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">RO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> loss, Environ. Sci. Technol., 56, 12926–12936, <ext-link xlink:href="https://doi.org/10.1021/acs.est.2c03628" ext-link-type="DOI">10.1021/acs.est.2c03628</ext-link>, 2022.</mixed-citation></ref>
      <ref id="bib1.bib30"><label>30</label><mixed-citation>Litfin, G., Pollock, C. R., Curl, R. F., and Tittel, F. K.: Sensitivity enhancement of laser absorption spectroscopy by magnetic rotation effect, J. Chem. Phys., 72, 6602–6605, <ext-link xlink:href="https://doi.org/10.1063/1.439117" ext-link-type="DOI">10.1063/1.439117</ext-link>, 1980.</mixed-citation></ref>
      <ref id="bib1.bib31"><label>31</label><mixed-citation>Liu, Y., Ivanov, A. V., and Molina, M. J.: Temperature dependence of OH diffusion in air and He, Geophys. Res. Lett., 36, L03816, <ext-link xlink:href="https://doi.org/10.1029/2008GL036170" ext-link-type="DOI">10.1029/2008GL036170</ext-link>, 2009.</mixed-citation></ref>
      <ref id="bib1.bib32"><label>32</label><mixed-citation>Lu, K., Guo, S., Tan, Z., Wang, H., Shang, D., Liu, Y., Li, X., Wu, Z., Hu, M., and Zhang, Y.: Exploring atmospheric free-radical chemistry in China: the self-cleansing capacity and the formation of secondary air pollution, Natl. Sci. Rev., 6, 579–594, <ext-link xlink:href="https://doi.org/10.1093/nsr/nwy073" ext-link-type="DOI">10.1093/nsr/nwy073</ext-link>, 2018.</mixed-citation></ref>
      <ref id="bib1.bib33"><label>33</label><mixed-citation>Lou, S., Holland, F., Rohrer, F., Lu, K., Bohn, B., Brauers, T., Chang, C. C., Fuchs, H., Häseler, R., Kita, K., Kondo, Y., Li, X., Shao, M., Zeng, L., Wahner, A., Zhang, Y., Wang, W., and Hofzumahaus, A.: Atmospheric OH reactivities in the Pearl River Delta – China in summer 2006: measurement and model results, Atmos. Chem. Phys., 10, 11243–11260, <ext-link xlink:href="https://doi.org/10.5194/acp-10-11243-2010" ext-link-type="DOI">10.5194/acp-10-11243-2010</ext-link>, 2010.</mixed-citation></ref>
      <ref id="bib1.bib34"><label>34</label><mixed-citation>Luo, P.: Long-wave mid-infrared time-resolved dual-comb spectroscopy of short-lived intermediates, Opt. Lett., 45, 6791–6794, <ext-link xlink:href="https://doi.org/10.1364/OL.413754" ext-link-type="DOI">10.1364/OL.413754</ext-link>, 2020.</mixed-citation></ref>
      <ref id="bib1.bib35"><label>35</label><mixed-citation>Luo, P. and Horng, E.: Simultaneous determination of transient free radicals and reaction kinetics by high-resolution time-resolved dual-comb spectroscopy, Commun. Chem., 3, 95, <ext-link xlink:href="https://doi.org/10.1038/s42004-020-00353-6" ext-link-type="DOI">10.1038/s42004-020-00353-6</ext-link>, 2020.</mixed-citation></ref>
      <ref id="bib1.bib36"><label>36</label><mixed-citation>Luo, P., Chung, C., and Lee, Y.: Rate coefficient of the reaction <inline-formula><mml:math id="M492" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">CH</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mi mathvariant="normal">OO</mml:mi></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M493" display="inline"><mml:mo>+</mml:mo></mml:math></inline-formula> <inline-formula><mml:math id="M494" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">NO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> probed with a quantum-cascade laser near 11 <inline-formula><mml:math id="M495" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi><mml:mi mathvariant="normal">m</mml:mi></mml:mrow></mml:math></inline-formula>, Phys. Chem. Chem. Phys., 21, 17578–17583, <ext-link xlink:href="https://doi.org/10.1039/C9CP03333E" ext-link-type="DOI">10.1039/C9CP03333E</ext-link>, 2019.</mixed-citation></ref>
      <ref id="bib1.bib37"><label>37</label><mixed-citation>Mao, J., Ren, X., Brune, W. H., Olson, J. R., Crawford, J. H., Fried, A., Huey, L. G., Cohen, R. C., Heikes, B., Singh, H. B., Blake, D. R., Sachse, G. W., Diskin, G. S., Hall, S. R., and Shetter, R. E.: Airborne measurement of OH reactivity during INTEX-B, Atmos. Chem. Phys., 9, 163–173, <ext-link xlink:href="https://doi.org/10.5194/acp-9-163-2009" ext-link-type="DOI">10.5194/acp-9-163-2009</ext-link>, 2009.</mixed-citation></ref>
      <ref id="bib1.bib38"><label>38</label><mixed-citation>Mao, J., Ren, X., Chen, S., Brune, W., Chen, Z., Martinez, M., Harder, H., Lefer, B., Rappenglück, B., Flynn, J., and Leuchner, M.: Atmospheric oxidation capacity in the summer of Houston 2006: comparison with summer measurements in other metropolitan studies, Atmos. Environ., 44, 4107–4115, <ext-link xlink:href="https://doi.org/10.1016/j.atmosenv.2009.01.013" ext-link-type="DOI">10.1016/j.atmosenv.2009.01.013</ext-link>, 2010.</mixed-citation></ref>
      <ref id="bib1.bib39"><label>39</label><mixed-citation>Martinez, M., Harder, H., Kovacs, T. A., Simpas, J. B., Bassis, J., Lesher, R., Brune, W. H., Frost, G. J., Williams, E. J., Stroud, C. A., Jobson, B. T., Roberts, J. M., Hall, S. R., Shetter, R. E., Wert, B., Fried, A., Alicke, B., Stutz, J., Young, V. L., White, A. B., and Zamora, R. J.: OH and <inline-formula><mml:math id="M496" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">HO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> concentrations, sources, and loss rates during the Southern Oxidants Study in Nashville, Tennessee, summer 1999, J. Geophys. Res., 108, 4617, <ext-link xlink:href="https://doi.org/10.1029/2003JD003551" ext-link-type="DOI">10.1029/2003JD003551</ext-link>, 2003.</mixed-citation></ref>
      <ref id="bib1.bib40"><label>40</label><mixed-citation>Michoud, V., Hansen, R. F., Locoge, N., Stevens, P. S., and Dusanter, S.: Detailed characterizations of the new Mines Douai comparative reactivity method instrument via laboratory experiments and modeling, Atmos. Meas. Tech., 8, 3537–3553, <ext-link xlink:href="https://doi.org/10.5194/amt-8-3537-2015" ext-link-type="DOI">10.5194/amt-8-3537-2015</ext-link>, 2015.</mixed-citation></ref>
      <ref id="bib1.bib41"><label>41</label><mixed-citation>Muller, J. B. A., Elste, T., Plass-Dülmer, C., Stange, G., Holla, R., Claude, A., Englert, J., Gilge, S., and Kubistin, D.: A novel semi-direct method to measure OH reactivity by chemical ionization mass spectrometry (CIMS), Atmos. Meas. Tech., 11, 4413–4433, <ext-link xlink:href="https://doi.org/10.5194/amt-11-4413-2018" ext-link-type="DOI">10.5194/amt-11-4413-2018</ext-link>, 2018.</mixed-citation></ref>
      <ref id="bib1.bib42"><label>42</label><mixed-citation>Nicely, J. M., Canty, T. P., Manyin, M., Oman, L. D., Salawitch, R. J., Steenrod, S. D., Strahan, S. E., and Strode, S. A.: Changes in Global Tropospheric OH Expected as a Result of Climate Change Over the Last Several Decades, J. Geophys. Res.-Atmos., 123, 10774–10795, <ext-link xlink:href="https://doi.org/10.1029/2018JD028388" ext-link-type="DOI">10.1029/2018JD028388</ext-link>, 2018.</mixed-citation></ref>
      <ref id="bib1.bib43"><label>43</label><mixed-citation>Nölscher, A. C., Sinha, V., Bockisch, S., Klüpfel, T., and Williams, J.: Total OH reactivity measurements using a new fast Gas Chromatographic Photo-Ionization Detector (GC-PID), Atmos. Meas. Tech., 5, 2981–2992, <ext-link xlink:href="https://doi.org/10.5194/amt-5-2981-2012" ext-link-type="DOI">10.5194/amt-5-2981-2012</ext-link>, 2012.</mixed-citation></ref>
      <ref id="bib1.bib44"><label>44</label><mixed-citation> Parker, A. E., Amedro, D., Schoemaecker, C., and Fittschen, C.: OH radical reactivity measurements by FAGE, Environ. Eng. Manag. J., 10, 107–114, 2011.</mixed-citation></ref>
      <ref id="bib1.bib45"><label>45</label><mixed-citation>Pilgrim, J. S., Jennings, R. T., and Taatjes, C. A.: Temperature controlled multiple pass absorption cell for gas phase chemical kinetics studies, Rev. Sci. Instrum., 68, 1875–1878, <ext-link xlink:href="https://doi.org/10.1063/1.1147960" ext-link-type="DOI">10.1063/1.1147960</ext-link>, 1997.</mixed-citation></ref>
      <ref id="bib1.bib46"><label>46</label><mixed-citation>Praplan, A. P., Pfannerstill, E., Williams, J., and Helen, H.: OH reactivity of the urban air in Helsinki, Finland, during winter, Atmos. Environ., 169, 150–161, <ext-link xlink:href="https://doi.org/10.1016/j.atmosenv.2017.09.013" ext-link-type="DOI">10.1016/j.atmosenv.2017.09.013</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib47"><label>47</label><mixed-citation>Qian, H., Turton, D., Seakins, P. W., and Pilling, M. J.: Dynamic frequency stabilization of infrared diode laser for kinetic studies, Chem. Phys. Lett., 322, 57–64, <ext-link xlink:href="https://doi.org/10.1016/S0009-2614(00)00395-X" ext-link-type="DOI">10.1016/S0009-2614(00)00395-X</ext-link>, 2000.</mixed-citation></ref>
      <ref id="bib1.bib48"><label>48</label><mixed-citation>Sadanaga, Y., Yoshino, A., Watanabe, K., Yoshioka, A., Wakazono, Y., Kanaya, Y., and Kajii, Y.: Development of a measurement system of OH reactivity in the atmosphere by using a laser-induced pump and probe technique, Rev. Sci. Instrum., 75, 2648–2655, <ext-link xlink:href="https://doi.org/10.1063/1.1775311" ext-link-type="DOI">10.1063/1.1775311</ext-link>, 2004.</mixed-citation></ref>
      <ref id="bib1.bib49"><label>49</label><mixed-citation>Safieddine, S. A., Heald, C. L., and Henderson, B. H.: The global nonmethane reactive organic carbon budget: A modeling perspective, Geophys. Res. Lett., 44, 3897–3906, <ext-link xlink:href="https://doi.org/10.1002/2017GL072602" ext-link-type="DOI">10.1002/2017GL072602</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib50"><label>50</label><mixed-citation>Schilt, S., Thévenaz, L., and Robert, P.: Wavelength modulation spectroscopy: combined frequency and intensity laser modulation, Appl. Optics, 42, 6728–6738, <ext-link xlink:href="https://doi.org/10.1364/AO.42.006728" ext-link-type="DOI">10.1364/AO.42.006728</ext-link>, 2003.</mixed-citation></ref>
      <ref id="bib1.bib51"><label>51</label><mixed-citation>Sinha, V., Williams, J., Crowley, J. N., and Lelieveld, J.: The Comparative Reactivity Method – a new tool to measure total OH Reactivity in ambient air, Atmos. Chem. Phys., 8, 2213–2227, <ext-link xlink:href="https://doi.org/10.5194/acp-8-2213-2008" ext-link-type="DOI">10.5194/acp-8-2213-2008</ext-link>, 2008.</mixed-citation></ref>
      <ref id="bib1.bib52"><label>52</label><mixed-citation>Sinha, V., Williams, J., Diesch, J. M., Drewnick, F., Martinez, M., Harder, H., Regelin, E., Kubistin, D., Bozem, H., Hosaynali-Beygi, Z., Fischer, H., Andrés-Hernández, M. D., Kartal, D., Adame, J. A., and Lelieveld, J.: Constraints on instantaneous ozone production rates and regimes during DOMINO derived using in-situ OH reactivity measurements, Atmos. Chem. Phys., 12, 7269–7283, <ext-link xlink:href="https://doi.org/10.5194/acp-12-7269-2012" ext-link-type="DOI">10.5194/acp-12-7269-2012</ext-link>, 2012.</mixed-citation></ref>
      <ref id="bib1.bib53"><label>53</label><mixed-citation>Song, B., Yan, X., Tan, S., Sai, B., Lai, S., Yu, H., Ou, C., and Lu, X.: Human mobility models reveal the underlying mechanism of seasonal movements across China, Int. J. Mod. Phys. C, 33, 2250054, <ext-link xlink:href="https://doi.org/10.1142/S0129183122500541" ext-link-type="DOI">10.1142/S0129183122500541</ext-link>, 2022.</mixed-citation></ref>
      <ref id="bib1.bib54"><label>54</label><mixed-citation>Stone, D., Whalley, L. K., and Heard, D. E.: Tropospheric OH and <inline-formula><mml:math id="M497" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">HO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> radicals: field measurements and model comparisons, Chem. Soc. Rev., 41, 6348–6404, <ext-link xlink:href="https://doi.org/10.1039/c2cs35140d" ext-link-type="DOI">10.1039/c2cs35140d</ext-link>, 2012.</mixed-citation></ref>
      <ref id="bib1.bib55"><label>55</label><mixed-citation>Stone, D., Whalley, L. K., Ingham, T., Edwards, P. M., Cryer, D. R., Brumby, C. A., Seakins, P. W., and Heard, D. E.: Measurement of OH reactivity by laser flash photolysis coupled with laser-induced fluorescence spectroscopy, Atmos. Meas. Tech., 9, 2827–2844, <ext-link xlink:href="https://doi.org/10.5194/amt-9-2827-2016" ext-link-type="DOI">10.5194/amt-9-2827-2016</ext-link>, 2016.</mixed-citation></ref>
      <ref id="bib1.bib56"><label>56</label><mixed-citation>Teng, C. C., Yan, C., Rousso, A., Zhong, H., Chen, T., Zhang, E. J., Ju, Y., and Wysocki, G.: Time-resolved <inline-formula><mml:math id="M498" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">HO</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula> detection with Faraday rotation spectroscopy in a photolysis reactor, Opt. Express, 29, 2769–2779, <ext-link xlink:href="https://doi.org/10.1364/OE.413063" ext-link-type="DOI">10.1364/OE.413063</ext-link>, 2021.</mixed-citation></ref>
      <ref id="bib1.bib57"><label>57</label><mixed-citation>Trutna, W. R. and Byer, R. L.: Multiple-pass Raman gain cell, Appl. Optics, 19, 301–312, <ext-link xlink:href="https://doi.org/10.1364/AO.19.000301" ext-link-type="DOI">10.1364/AO.19.000301</ext-link>, 1980.</mixed-citation></ref>
      <ref id="bib1.bib58"><label>58</label><mixed-citation>Wang, W., Li, X., Cheng, Y., Parrish, D. D., Ni, R., Tan, Z., Liu, Y., Lu, S., Wu, Y., Chen, S., Lu, K., Hu, M., Zeng, L., Shao, M., Huang, C., Tian, X., Leung, K. M., Chen, L., Fan, M., Zhang, Q., Rohrer, F., Wahner, A., Pöschl, U., Su, H., and Zhang, Y.: Ozone pollution mitigation strategy informed by long-term trends of atmospheric oxidation capacity, Nat. Geosci., 17, 20–25, <ext-link xlink:href="https://doi.org/10.1038/s41561-023-01334-9" ext-link-type="DOI">10.1038/s41561-023-01334-9</ext-link>, 2023.</mixed-citation></ref>
      <ref id="bib1.bib59"><label>59</label><mixed-citation>Wei, N., Fang, B., Zhao, W., Wang, C., Yang, N., Zhang, W., Chen, W., and Fittschen, C.: Time-resolved laser-flash photolysis Faraday rotation spectrometer: a new tool for total OH reactivity measurement and free radical kinetics research, Anal. Chem., 92, 4334–4339, <ext-link xlink:href="https://doi.org/10.1021/acs.analchem.9b05117" ext-link-type="DOI">10.1021/acs.analchem.9b05117</ext-link>, 2020.</mixed-citation></ref>
      <ref id="bib1.bib60"><label>60</label><mixed-citation>Wei, N., Zhao, W., Yao, Y., Wang, H., Liu, Z., Xu, X., Rahman, M., Zhang, C., Fittschen, C., and Zhang, W.: Peroxy radical chemistry during ozone photochemical pollution season at a suburban site in the boundary of Jiangsu–Anhui–Shandong–Henan region, China, Sci. Total Environ., 904, 166355, <ext-link xlink:href="https://doi.org/10.1016/j.scitotenv.2023.166355" ext-link-type="DOI">10.1016/j.scitotenv.2023.166355</ext-link>, 2023.</mixed-citation></ref>
      <ref id="bib1.bib61"><label>61</label><mixed-citation>Westberg, J. and Axner, O.: Lineshape asymmetries in Faraday modulation spectroscopy, Appl. Phys. B, 116, 467–476, <ext-link xlink:href="https://doi.org/10.1007/s00340-013-5721-x" ext-link-type="DOI">10.1007/s00340-013-5721-x</ext-link>, 2014. </mixed-citation></ref>
      <ref id="bib1.bib62"><label>62</label><mixed-citation>Wolfe, G. M., Marvin, M. R., Roberts, S. J., Travis, K. R., and Liao, J.: The Framework for 0-D Atmospheric Modeling (F0AM) v3.1, Geosci. Model Dev., 9, 3309–3319, <ext-link xlink:href="https://doi.org/10.5194/gmd-9-3309-2016" ext-link-type="DOI">10.5194/gmd-9-3309-2016</ext-link>, 2016.</mixed-citation></ref>
      <ref id="bib1.bib63"><label>63</label><mixed-citation>Yan, C., Teng, C. C., Chen, T., Zhong, H., Rousso, A., Zhao, H., Ma, G., Wysocki, G., and Ju, Y.: The kinetic study of excited singlet oxygen atom <inline-formula><mml:math id="M499" display="inline"><mml:mrow class="chem"><mml:mi mathvariant="normal">O</mml:mi><mml:msup><mml:mo>(</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:msup><mml:mi mathvariant="normal">D</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:math></inline-formula> reactions with acetylene, Combust. Flame, 212, 135–141, <ext-link xlink:href="https://doi.org/10.1016/j.combustflame.2019.10.034" ext-link-type="DOI">10.1016/j.combustflame.2019.10.034</ext-link>, 2020.</mixed-citation></ref>
      <ref id="bib1.bib64"><label>64</label><mixed-citation>Yang, Y., Shao, M., Wang, X., Nölscher, A. C., Kessel, S., Guenther, A., and Williams, J.: Towards a quantitative understanding of total OH reactivity: A review, Atmos. Environ., 134, 147–161, <ext-link xlink:href="https://doi.org/10.1016/j.atmosenv.2016.03.010" ext-link-type="DOI">10.1016/j.atmosenv.2016.03.010</ext-link>, 2016.</mixed-citation></ref>
      <ref id="bib1.bib65"><label>65</label><mixed-citation>Yang, Y., Shao, M., Keßel, S., Li, Y., Lu, K., Lu, S., Williams, J., Zhang, Y., Zeng, L., Nölscher, A. C., Wu, Y., Wang, X., and Zheng, J.: How the OH reactivity affects the ozone production efficiency: case studies in Beijing and Heshan, China, Atmos. Chem. Phys., 17, 7127–7142, <ext-link xlink:href="https://doi.org/10.5194/acp-17-7127-2017" ext-link-type="DOI">10.5194/acp-17-7127-2017</ext-link>, 2017.</mixed-citation></ref>
      <ref id="bib1.bib66"><label>66</label><mixed-citation>Zannoni, N., Dusanter, S., Gros, V., Sarda Esteve, R., Michoud, V., Sinha, V., Locoge, N., and Bonsang, B.: Intercomparison of two comparative reactivity method instruments inf the Mediterranean basin during summer 2013, Atmos. Meas. Tech., 8, 3851–3865, <ext-link xlink:href="https://doi.org/10.5194/amt-8-3851-2015" ext-link-type="DOI">10.5194/amt-8-3851-2015</ext-link>, 2015.</mixed-citation></ref>
      <ref id="bib1.bib67"><label>67</label><mixed-citation>Zhao, W., Wysocki, G., Chen, W., Fertein, E., Coq, L. D., Petiprez, D., and Zhang, W.: Sensitive and selective detection of OH radicals using Faraday rotation spectroscopy at 2.8 <inline-formula><mml:math id="M500" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi><mml:mi mathvariant="normal">m</mml:mi></mml:mrow></mml:math></inline-formula>, Opt. Express, 19, 2493–2501, <ext-link xlink:href="https://doi.org/10.1364/OE.19.002493" ext-link-type="DOI">10.1364/OE.19.002493</ext-link>, 2011.</mixed-citation></ref>
      <ref id="bib1.bib68"><label>68</label><mixed-citation>Zhao, W., Wyscoki, G., Chen, W., Zhang, W.: High sensitivity Faraday rotation spectrometer for hydroxyl radical detection at 2.8 <inline-formula><mml:math id="M501" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi><mml:mi mathvariant="normal">m</mml:mi></mml:mrow></mml:math></inline-formula>, Appl. Phys. B, 109, 511–519, <ext-link xlink:href="https://doi.org/10.1007/s00340-012-5089-3" ext-link-type="DOI">10.1007/s00340-012-5089-3</ext-link>, 2012.</mixed-citation></ref>
      <ref id="bib1.bib69"><label>69</label><mixed-citation>Zhao, W., Fang, B., Lin, X., Gai, Y., Zhang, W., Chen, W., Chen, Z., Zhang, H., and Chen, W.: Superconducting-magnet-based Faraday rotation spectrometer for real time in situ measurement of OH radicals at 10<sup>6</sup> <inline-formula><mml:math id="M503" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">molecule</mml:mi><mml:mo>/</mml:mo><mml:msup><mml:mi mathvariant="normal">cm</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:mrow></mml:math></inline-formula> level in an atmospheric simulation chamber, Anal. Chem., 90, 3958–3964, <ext-link xlink:href="https://doi.org/10.1021/acs.analchem.7b04949" ext-link-type="DOI">10.1021/acs.analchem.7b04949</ext-link>, 2018.</mixed-citation></ref>

  </ref-list></back>
    <!--<article-title-html>Development of a portable laser-flash photolysis Faraday rotation spectrometer for measuring atmospheric total OH reactivity</article-title-html>
<abstract-html/>
<ref-html id="bib1.bib1"><label>1</label><mixed-citation>
      
Atkinson, R., Baulch, D. L., Cox, R. A., Crowley, J. N., Hampson, R. F., Hynes, R. G., Jenkin, M. E., Rossi, M. J., and Troe, J.:
Evaluated kinetic and photochemical data for atmospheric chemistry: Volume I – gas phase reactions of O<sub>x</sub>, HO<sub>x</sub>, NO<sub>x</sub> and SO<sub>x</sub> species, Atmos. Chem. Phys., 4, 1461–1738, <a href="https://doi.org/10.5194/acp-4-1461-2004" target="_blank">https://doi.org/10.5194/acp-4-1461-2004</a>, 2004.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib2"><label>2</label><mixed-citation>
      
Atkinson, R., Baulch, D. L., Cox, R. A., Crowley, J. N., Hampson, R. F., Hynes, R. G., Jenkin, M. E., Rossi, M. J., Troe, J., and IUPAC Subcommittee:
Evaluated kinetic and photochemical data for atmospheric chemistry: Volume II – gas phase reactions of organic species, Atmos. Chem. Phys., 6, 3625–4055, <a href="https://doi.org/10.5194/acp-6-3625-2006" target="_blank">https://doi.org/10.5194/acp-6-3625-2006</a>, 2006.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib3"><label>3</label><mixed-citation>
      
Brecha, R. J., Pedrotti, L. M., and Krause, D.:
Magnetic rotation spectroscopy of molecular oxygen with a diode laser, J. Opt. Soc. Am. B, 14, 1921–1930, <a href="https://doi.org/10.1063/1.1149176" target="_blank">https://doi.org/10.1063/1.1149176</a>, 1997.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib4"><label>4</label><mixed-citation>
      
Cheng, F., Zhao, W., Fang, B., Zhang, Y., Yang, N., Zhou, H., and Zhang, W.:
High band-width mid-infrared frequency-modulated Faraday rotation spectrometer for time resolved measurement of the OH radical, Opt. Express, 31, 25058–25069, <a href="https://doi.org/10.1364/OE.493270" target="_blank">https://doi.org/10.1364/OE.493270</a>, 2023.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib5"><label>5</label><mixed-citation>
      
Di Carlo, P., Brune, W. H., Martinez, M., Harder, H., Lesher, R., Ren, X., Thornberry, T., Carroll, M. A., Young, V., Shepson, P. B., Riemer, D., Apel, E., and Campbell, C.:
Missing OH reactivity in a forest: evidence for unknown reactive biogenic VOCs, Science, 304, 722–725, <a href="https://doi.org/10.1126/science.1094392" target="_blank">https://doi.org/10.1126/science.1094392</a>, 2004.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib6"><label>6</label><mixed-citation>
      
Fang, B., Yang, N., Wang, C., Zhao, W., Xu, X., Zhang, Y., and Zhang, W.:
Detection of nitric oxide with Faraday rotation spectroscopy at 5.33&thinsp;µm, Chin. J. Chem. Phys., 33, 37–42, <a href="https://doi.org/10.1063/1674-0068/cjcp1910182" target="_blank">https://doi.org/10.1063/1674-0068/cjcp1910182</a>, 2020.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib7"><label>7</label><mixed-citation>
      
Fang, B.,
Wei, N.,
Zhao, W.,
Yang, N.,
Zhou, H.,
Zhang, H.,
Li, J.,
Zhang, W.,
Lu, Y.,
Zhu, Z.,
and Liu, Y.: Data used in preprint of “Development of a portable laser-flash photolysis Faraday rotation spectrometer for measuring atmospheric total OH reactivity” [DS/OL], V1, Science Data Bank [data set], <a href="https://doi.org/10.57760/sciencedb.19568" target="_blank">https://doi.org/10.57760/sciencedb.19568</a>, 2025.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib8"><label>8</label><mixed-citation>
      
Fatahi, Y., Kouznetsov, R., and Sofiev, M.:
The effect of accounting for public holidays on the skills of the atmospheric composition model SILAM v.5.7, Geosci. Model Dev., 14, 7459–7475, <a href="https://doi.org/10.5194/gmd-14-7459-2021" target="_blank">https://doi.org/10.5194/gmd-14-7459-2021</a>, 2021.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib9"><label>9</label><mixed-citation>
      
Fuchs, H., Hofzumahaus, A., Rohrer, F., Bohn, B., Brauers, T., Dorn, H. P., Häseler, R., Holland, F., Kaminski, M., Li, X., Lu, K., Nehr, S., Tillmann, R., Wegener, R., and Wahner, A.:
Experimental evidence for efficient hydroxyl radical regeneration in isoprene oxidation, Nat. Geosci., 6, 1023–1026, <a href="https://doi.org/10.1038/ngeo1964" target="_blank">https://doi.org/10.1038/ngeo1964</a>, 2013.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib10"><label>10</label><mixed-citation>
      
Fuchs, H., Novelli, A., Rolletter, M., Hofzumahaus, A., Pfannerstill, E. Y., Kessel, S., Edtbauer, A., Williams, J., Michoud, V., Dusanter, S., Locoge, N., Zannoni, N., Gros, V., Truong, F., Sarda-Esteve, R., Cryer, D. R., Brumby, C. A., Whalley, L. K., Stone, D., Seakins, P. W., Heard, D. E., Schoemaecker, C., Blocquet, M., Coudert, S., Batut, S., Fittschen, C., Thames, A. B., Brune, W. H., Ernest, C., Harder, H., Muller, J. B. A., Elste, T., Kubistin, D., Andres, S., Bohn, B., Hohaus, T., Holland, F., Li, X., Rohrer, F., Kiendler-Scharr, A., Tillmann, R., Wegener, R., Yu, Z., Zou, Q., and Wahner, A.:
Comparison of OH reactivity measurements in the atmospheric simulation chamber SAPHIR, Atmos. Meas. Tech., 10, 4023–4053, <a href="https://doi.org/10.5194/amt-10-4023-2017" target="_blank">https://doi.org/10.5194/amt-10-4023-2017</a>, 2017.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib11"><label>11</label><mixed-citation>
      
Goldstein, A. H. and Galbally, I. E.:
Known and unexplored organic constituents in the Earth's atmosphere, Environ. Sci. Technol., 41, 1514–1521, <a href="https://doi.org/10.1021/es072476p" target="_blank">https://doi.org/10.1021/es072476p</a>, 2007.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib12"><label>12</label><mixed-citation>
      
Gordon, I. E., Rothman, L. S., Hargreaves, R. J., Hashemi, R., Karlovets, E. V., Skinner, F. M., Conway, E. K., Hill, C., Kochanov, R. V., Tan, Y., Wcisło, P., Finenko, A. A., Nelson, K., Bernath, P. F., Birk, M., Boudon, V., Campargue, A., Chance, K. V., Coustenis, A., Drouin, B. J., Flaud, J. M., Gamache, R. R., Hodges, J. T., Jacquemart, D., Mlawer, E. J., Nikitin, A. V., Perevalov, V. I., Rotger, M., Tennyson, J., Toon, G. C., Tran, H., Tyuterev, V. G., Adkins, E. M., Baker, A., Barbe, A., Canè, E., Császár, A. G., Dudaryonok, A., Egorov, O., Fleisher, A. J., Fleurbaey, H., Foltynowicz, A., Furtenbacher, T., Harrison, J. J., Hartmann, J. M., Horneman, V. M., Huang, X., Karman, T., Karns, J., Kassi, S., Kleiner, I., Kofman, V., Kwabia-Tchana, F., Lavrentieva, N. N., Lee, T. J., Long, D. A., Lukashevskaya, A. A., Lyulin, O. M., Makhnev, V. Y., Matt, W., Massie, S. T., Melosso, M., Mikhailenko, S. N., Mondelain, D., Müller, H. S. P., Naumenko, O. V., Perrin, A., Polyansky, O. L., Raddaoui, E., Raston, P. L., Reed, Z. D., Rey, M., Richard, C., Tóbiás, R., Sadiek, I., Schwenke, D. W., Starikova, E., Sung, K., Tamassia, F., Tashkun, S. A., Auwera, J. V., Vasilenko, I. A., Vigasin, A. A., Villanueva, G. L., Vispoel, B., Wagner, G., Yachmenev, A., and Yurchenko, S. N.:
The HITRAN2020 molecular spectroscopic database, J. Quant. Spectrosc. Ra., 277, 107949, <a href="https://doi.org/10.1016/j.jqsrt.2021.107949" target="_blank">https://doi.org/10.1016/j.jqsrt.2021.107949</a>, 2022.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib13"><label>13</label><mixed-citation>
      
Hansen, R. F., Griffith, S. M., Dusanter, S., Rickly, P. S., Stevens, P. S., Bertman, S. B., Carroll, M. A., Erickson, M. H., Flynn, J. H., Grossberg, N., Jobson, B. T., Lefer, B. L., and Wallace, H. W.:
Measurements of total hydroxyl radical reactivity during CABINEX 2009 – Part 1: field measurements, Atmos. Chem. Phys., 14, 2923–2937, <a href="https://doi.org/10.5194/acp-14-2923-2014" target="_blank">https://doi.org/10.5194/acp-14-2923-2014</a>, 2014.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib14"><label>14</label><mixed-citation>
      
Hansen, R. F., Blocquet, M., Schoemaecker, C., Léonardis, T., Locoge, N., Fittschen, C., Hanoune, B., Stevens, P. S., Sinha, V., and Dusanter, S.:
Intercomparison of the comparative reactivity method (CRM) and pump–probe technique for measuring total OH reactivity in an urban environment, Atmos. Meas. Tech., 8, 4243–4264, <a href="https://doi.org/10.5194/amt-8-4243-2015" target="_blank">https://doi.org/10.5194/amt-8-4243-2015</a>, 2015.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib15"><label>15</label><mixed-citation>
      
Heald, C. L., de Gouw, J., Goldstein, A. H., Guenther, A. B., Hayes, P. L., Hu, W., Isaacman-VanWertz, G., Jimenez, J. L., Keutsch, F. N., Koss, A. R., Misztal, P. K., Rappenglück, B., Roberts, J. M., Stevens, P. S., Washenfelder, R. A., Warneke, C., and Young, C. J.:
Contrasting reactive organic carbon observations in the southeast United States (SOAS) and southern California (CalNex), Environ. Sci. Technol., 54, 14923–14935, <a href="https://doi.org/10.1021/acs.est.0c05027" target="_blank">https://doi.org/10.1021/acs.est.0c05027</a>, 2020.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib16"><label>16</label><mixed-citation>
      
Hens, K., Novelli, A., Martinez, M., Auld, J., Axinte, R., Bohn, B., Fischer, H., Keronen, P., Kubistin, D., Nölscher, A. C., Oswald, R., Paasonen, P., Petäjä, T., Regelin, E., Sander, R., Sinha, V., Sipilä, M., Taraborrelli, D., Tatum Ernest, C., Williams, J., Lelieveld, J., and Harder, H.:
Observation and modelling of HO<sub>x</sub> radicals in a boreal forest, Atmos. Chem. Phys., 14, 8723–8747, <a href="https://doi.org/10.5194/acp-14-8723-2014" target="_blank">https://doi.org/10.5194/acp-14-8723-2014</a>, 2014.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib17"><label>17</label><mixed-citation>
      
Hunter, J. F., Day, D. A., Palm, B. B., Yatavelli, R. L. N., Chan, A. W. H., Kaser, L., Cappellin, L., Hayes, P. L., Cross, E. S., Carrasquillo, A. J., Campuzano-Jost, P., Stark, H., Zhao, Y., Hohaus, T., Smith, J. N., Hansel, A., Karl, T., Goldstein, A. H., Guenther, A., Worsnop, D. R., Thornton, J. A., Heald, C. L., Jimenez, J. L., and Kroll, J. H.:
Comprehensive characterization of atmospheric organic carbon at a forested site, Nat. Geosci., 10, 748–753, <a href="https://doi.org/10.1038/NGEO3018" target="_blank">https://doi.org/10.1038/NGEO3018</a>, 2017.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib18"><label>18</label><mixed-citation>
      
Ingham, T., Goddard, A., Whalley, L. K., Furneaux, K. L., Edwards, P. M., Seal, C. P., Self, D. E., Johnson, G. P., Read, K. A., Lee, J. D., and Heard, D. E.:
A flow-tube based laser-induced fluorescence instrument to measure OH reactivity in the troposphere, Atmos. Meas. Tech., 2, 465–477, <a href="https://doi.org/10.5194/amt-2-465-2009" target="_blank">https://doi.org/10.5194/amt-2-465-2009</a>, 2009.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib19"><label>19</label><mixed-citation>
      
Ivanov, A. V., Trakhtenberg, S., Bertram, A. K., Gershenzon, Y. M., and Molina, M. J.:
OH, HO<sub>2</sub>, and ozone gaseous diffusion coefficients, J. Phys. Chem. A, 111, 1632–1637, <a href="https://doi.org/10.1021/jp066558w" target="_blank">https://doi.org/10.1021/jp066558w</a>, 2007.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib20"><label>20</label><mixed-citation>
      
Khayyam, J., Xie, P., Xu, J., Tian, X., Feng, H., and Qinjin, W.:
Vertically resolved meteorological adjustments of aerosols and trace gases in Beijing, Taiyuan, and Hefei by using RF model, Sci. Total Environ., 948, 174795, <a href="https://doi.org/10.1016/j.scitotenv.2024.174795" target="_blank">https://doi.org/10.1016/j.scitotenv.2024.174795</a>, 2024.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib21"><label>21</label><mixed-citation>
      
Kim, S., Sanchez, D., Wang, M., Seco, R., Jeong, D., Hughes, S., Barletta, B., Blake, D. R., Jung, J., Kim, D., Lee, G., Lee, M., Ahn, J., Lee, S.-D., Cho, G., Sung, M. Y., Lee, Y. H., Kim, D. B., Kim, Y., Woo, J. H., Jo, D., Park, R., Park, J. H., Hong, Y. D., and Hong, J. H.:
OH reactivity in urban and suburban regions in Seoul, South Korea – an East Asian megacity in a rapid transition, Faraday Discuss., 189, 231–251, <a href="https://doi.org/10.1039/C5FD00230C" target="_blank">https://doi.org/10.1039/C5FD00230C</a>, 2016.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib22"><label>22</label><mixed-citation>
      
Kohno, N., Zhou, J., Li, J., Takemura, M., Ono, N., Sadanaga, Y., Nakashima, Y., Sato, K., Kato, S., Sakamoto, Y., and Kajii, Y.:
Impacts of missing OH reactivity and aerosol uptake of HO<sub>2</sub> radicals on tropospheric O<sub>3</sub> production during the AQUAS-Kyoto summer campaign in 2018, Atmos. Environ., 281, 119130, <a href="https://doi.org/10.1016/j.atmosenv.2022.119130" target="_blank">https://doi.org/10.1016/j.atmosenv.2022.119130</a>, 2022.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib23"><label>23</label><mixed-citation>
      
Kovacs, T. A. and Brune, W. H.:
Total OH loss rate measurement, J. Atmos. Chem., 39, 105–122, <a href="https://doi.org/10.1023/A:1010614113786" target="_blank">https://doi.org/10.1023/A:1010614113786</a>, 2001.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib24"><label>24</label><mixed-citation>
      
Kumar, V. and Sinha, V.:
VOC-OHM: A new technique for rapid measurements of ambient total OH reactivity and volatile organic compounds using a single proton transfer reaction mass spectrometer, Int. J. Mass Spectrom., 374, 55–63, <a href="https://doi.org/10.1016/j.ijms.2014.10.012" target="_blank">https://doi.org/10.1016/j.ijms.2014.10.012</a>, 2014.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib25"><label>25</label><mixed-citation>
      
Lawrence, M. G.:
The relationship between relative humidity and the dewpoint temperature in moist air, B. Am. Meteorol. Soc., 86, 225–234, <a href="https://doi.org/10.1175/BAMS-86-2-225" target="_blank">https://doi.org/10.1175/BAMS-86-2-225</a>, 2005.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib26"><label>26</label><mixed-citation>
      
Lewicki, R., Doty III, J. H., Curl, R. F., Tittel, F. K., and Wysocki, G.:
Ultrasensitive detection of nitric oxide at 5.33&thinsp;µm by using external cavity quantum cascade laser-based Faraday rotation spectroscopy, P. Natl. Acad. Sci. USA, 106, 12587–12592, <a href="https://doi.org/10.1073/pnas.0906291106" target="_blank">https://doi.org/10.1073/pnas.0906291106</a>, 2009.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib27"><label>27</label><mixed-citation>
      
Lewis, T., Heard, D. E., and Blitz, M. A.:
A novel multiplex absorption spectrometer for time-resolved studies, Rev. Sci. Instrum., 89, 024101, <a href="https://doi.org/10.1063/1.5006539" target="_blank">https://doi.org/10.1063/1.5006539</a>, 2018.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib28"><label>28</label><mixed-citation>
      
Li, J., Kohno, N., Sakamoto, Y., Fukusaki, Y., Kousa, Y., Sadanaga, Y., Nakashima, Y., Sato, K., Ramasamy, S., Takami, A., Yoshino, A., Nakayama, T., Kato, S., Ono, N., Zhou, J., Bai, Y., and Kajii, Y.:
A quantitative understanding of total OH reactivity and ozone production in a coastal industrial area during the Yokohama air quality study (AQUAS) campaign of summer 2019, Atmos. Environ., 267, 118754, <a href="https://doi.org/10.1016/j.atmosenv.2021.118754" target="_blank">https://doi.org/10.1016/j.atmosenv.2021.118754</a>, 2021.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib29"><label>29</label><mixed-citation>
      
Li, J., Kohno, N., Sakamoto, Y., Pham, H. G., Murano, K., Sato, K., Nakayama, T., and Kajii, Y.:
Potential factors contributing to ozone production in AQUAS-Kyoto campaign in summer 2020: natural source-related missing OH reactivity and heterogeneous HO<sub>2</sub>/RO<sub>2</sub> loss, Environ. Sci. Technol., 56, 12926–12936, <a href="https://doi.org/10.1021/acs.est.2c03628" target="_blank">https://doi.org/10.1021/acs.est.2c03628</a>, 2022.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib30"><label>30</label><mixed-citation>
      
Litfin, G., Pollock, C. R., Curl, R. F., and Tittel, F. K.:
Sensitivity enhancement of laser absorption spectroscopy by magnetic rotation effect, J. Chem. Phys., 72, 6602–6605, <a href="https://doi.org/10.1063/1.439117" target="_blank">https://doi.org/10.1063/1.439117</a>, 1980.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib31"><label>31</label><mixed-citation>
      
Liu, Y., Ivanov, A. V., and Molina, M. J.:
Temperature dependence of OH diffusion in air and He, Geophys. Res. Lett., 36, L03816, <a href="https://doi.org/10.1029/2008GL036170" target="_blank">https://doi.org/10.1029/2008GL036170</a>, 2009.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib32"><label>32</label><mixed-citation>
      
Lu, K., Guo, S., Tan, Z., Wang, H., Shang, D., Liu, Y., Li, X., Wu, Z., Hu, M., and Zhang, Y.:
Exploring atmospheric free-radical chemistry in China: the self-cleansing capacity and the formation of secondary air pollution, Natl. Sci. Rev., 6, 579–594, <a href="https://doi.org/10.1093/nsr/nwy073" target="_blank">https://doi.org/10.1093/nsr/nwy073</a>, 2018.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib33"><label>33</label><mixed-citation>
      
Lou, S., Holland, F., Rohrer, F., Lu, K., Bohn, B., Brauers, T., Chang, C. C., Fuchs, H., Häseler, R., Kita, K., Kondo, Y., Li, X., Shao, M., Zeng, L., Wahner, A., Zhang, Y., Wang, W., and Hofzumahaus, A.:
Atmospheric OH reactivities in the Pearl River Delta – China in summer 2006: measurement and model results, Atmos. Chem. Phys., 10, 11243–11260, <a href="https://doi.org/10.5194/acp-10-11243-2010" target="_blank">https://doi.org/10.5194/acp-10-11243-2010</a>, 2010.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib34"><label>34</label><mixed-citation>
      
Luo, P.:
Long-wave mid-infrared time-resolved dual-comb spectroscopy of short-lived intermediates, Opt. Lett., 45, 6791–6794, <a href="https://doi.org/10.1364/OL.413754" target="_blank">https://doi.org/10.1364/OL.413754</a>, 2020.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib35"><label>35</label><mixed-citation>
      
Luo, P. and Horng, E.:
Simultaneous determination of transient free radicals and reaction kinetics by high-resolution time-resolved dual-comb spectroscopy, Commun. Chem., 3, 95, <a href="https://doi.org/10.1038/s42004-020-00353-6" target="_blank">https://doi.org/10.1038/s42004-020-00353-6</a>, 2020.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib36"><label>36</label><mixed-citation>
      
Luo, P., Chung, C., and Lee, Y.:
Rate coefficient of the reaction CH<sub>2</sub>OO&thinsp;+&thinsp;NO<sub>2</sub> probed with a quantum-cascade laser near 11&thinsp;µm, Phys. Chem. Chem. Phys., 21, 17578–17583, <a href="https://doi.org/10.1039/C9CP03333E" target="_blank">https://doi.org/10.1039/C9CP03333E</a>, 2019.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib37"><label>37</label><mixed-citation>
      
Mao, J., Ren, X., Brune, W. H., Olson, J. R., Crawford, J. H., Fried, A., Huey, L. G., Cohen, R. C., Heikes, B., Singh, H. B., Blake, D. R., Sachse, G. W., Diskin, G. S., Hall, S. R., and Shetter, R. E.:
Airborne measurement of OH reactivity during INTEX-B, Atmos. Chem. Phys., 9, 163–173, <a href="https://doi.org/10.5194/acp-9-163-2009" target="_blank">https://doi.org/10.5194/acp-9-163-2009</a>, 2009.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib38"><label>38</label><mixed-citation>
      
Mao, J., Ren, X., Chen, S., Brune, W., Chen, Z., Martinez, M., Harder, H., Lefer, B., Rappenglück, B., Flynn, J., and Leuchner, M.:
Atmospheric oxidation capacity in the summer of Houston 2006: comparison with summer measurements in other metropolitan studies, Atmos. Environ., 44, 4107–4115, <a href="https://doi.org/10.1016/j.atmosenv.2009.01.013" target="_blank">https://doi.org/10.1016/j.atmosenv.2009.01.013</a>, 2010.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib39"><label>39</label><mixed-citation>
      
Martinez, M., Harder, H., Kovacs, T. A., Simpas, J. B., Bassis, J., Lesher, R., Brune, W. H., Frost, G. J., Williams, E. J., Stroud, C. A., Jobson, B. T., Roberts, J. M., Hall, S. R., Shetter, R. E., Wert, B., Fried, A., Alicke, B., Stutz, J., Young, V. L., White, A. B., and Zamora, R. J.:
OH and HO<sub>2</sub> concentrations, sources, and loss rates during the Southern Oxidants Study in Nashville, Tennessee, summer 1999, J. Geophys. Res., 108, 4617, <a href="https://doi.org/10.1029/2003JD003551" target="_blank">https://doi.org/10.1029/2003JD003551</a>, 2003.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib40"><label>40</label><mixed-citation>
      
Michoud, V., Hansen, R. F., Locoge, N., Stevens, P. S., and Dusanter, S.:
Detailed characterizations of the new Mines Douai comparative reactivity method instrument via laboratory experiments and modeling, Atmos. Meas. Tech., 8, 3537–3553, <a href="https://doi.org/10.5194/amt-8-3537-2015" target="_blank">https://doi.org/10.5194/amt-8-3537-2015</a>, 2015.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib41"><label>41</label><mixed-citation>
      
Muller, J. B. A., Elste, T., Plass-Dülmer, C., Stange, G., Holla, R., Claude, A., Englert, J., Gilge, S., and Kubistin, D.:
A novel semi-direct method to measure OH reactivity by chemical ionization mass spectrometry (CIMS), Atmos. Meas. Tech., 11, 4413–4433, <a href="https://doi.org/10.5194/amt-11-4413-2018" target="_blank">https://doi.org/10.5194/amt-11-4413-2018</a>, 2018.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib42"><label>42</label><mixed-citation>
      
Nicely, J. M., Canty, T. P., Manyin, M., Oman, L. D., Salawitch, R. J., Steenrod, S. D., Strahan, S. E., and Strode, S. A.:
Changes in Global Tropospheric OH Expected as a Result of Climate Change Over the Last Several Decades, J. Geophys. Res.-Atmos., 123, 10774–10795, <a href="https://doi.org/10.1029/2018JD028388" target="_blank">https://doi.org/10.1029/2018JD028388</a>, 2018.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib43"><label>43</label><mixed-citation>
      
Nölscher, A. C., Sinha, V., Bockisch, S., Klüpfel, T., and Williams, J.:
Total OH reactivity measurements using a new fast Gas Chromatographic Photo-Ionization Detector (GC-PID), Atmos. Meas. Tech., 5, 2981–2992, <a href="https://doi.org/10.5194/amt-5-2981-2012" target="_blank">https://doi.org/10.5194/amt-5-2981-2012</a>, 2012.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib44"><label>44</label><mixed-citation>
      
Parker, A. E., Amedro, D., Schoemaecker, C., and Fittschen, C.:
OH radical reactivity measurements by FAGE, Environ. Eng. Manag. J., 10, 107–114, 2011.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib45"><label>45</label><mixed-citation>
      
Pilgrim, J. S., Jennings, R. T., and Taatjes, C. A.:
Temperature controlled multiple pass absorption cell for gas phase chemical kinetics studies, Rev. Sci. Instrum., 68, 1875–1878, <a href="https://doi.org/10.1063/1.1147960" target="_blank">https://doi.org/10.1063/1.1147960</a>, 1997.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib46"><label>46</label><mixed-citation>
      
Praplan, A. P., Pfannerstill, E., Williams, J., and Helen, H.:
OH reactivity of the urban air in Helsinki, Finland, during winter, Atmos. Environ., 169, 150–161, <a href="https://doi.org/10.1016/j.atmosenv.2017.09.013" target="_blank">https://doi.org/10.1016/j.atmosenv.2017.09.013</a>, 2017.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib47"><label>47</label><mixed-citation>
      
Qian, H., Turton, D., Seakins, P. W., and Pilling, M. J.:
Dynamic frequency stabilization of infrared diode laser for kinetic studies, Chem. Phys. Lett., 322, 57–64, <a href="https://doi.org/10.1016/S0009-2614(00)00395-X" target="_blank">https://doi.org/10.1016/S0009-2614(00)00395-X</a>, 2000.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib48"><label>48</label><mixed-citation>
      
Sadanaga, Y., Yoshino, A., Watanabe, K., Yoshioka, A., Wakazono, Y., Kanaya, Y., and Kajii, Y.:
Development of a measurement system of OH reactivity in the atmosphere by using a laser-induced pump and probe technique, Rev. Sci. Instrum., 75, 2648–2655, <a href="https://doi.org/10.1063/1.1775311" target="_blank">https://doi.org/10.1063/1.1775311</a>, 2004.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib49"><label>49</label><mixed-citation>
      
Safieddine, S. A., Heald, C. L., and Henderson, B. H.:
The global nonmethane reactive organic carbon budget: A modeling perspective, Geophys. Res. Lett., 44, 3897–3906, <a href="https://doi.org/10.1002/2017GL072602" target="_blank">https://doi.org/10.1002/2017GL072602</a>, 2017.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib50"><label>50</label><mixed-citation>
      
Schilt, S., Thévenaz, L., and Robert, P.:
Wavelength modulation spectroscopy: combined frequency and intensity laser modulation, Appl. Optics, 42, 6728–6738, <a href="https://doi.org/10.1364/AO.42.006728" target="_blank">https://doi.org/10.1364/AO.42.006728</a>, 2003.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib51"><label>51</label><mixed-citation>
      
Sinha, V., Williams, J., Crowley, J. N., and Lelieveld, J.:
The Comparative Reactivity Method – a new tool to measure total OH Reactivity in ambient air, Atmos. Chem. Phys., 8, 2213–2227, <a href="https://doi.org/10.5194/acp-8-2213-2008" target="_blank">https://doi.org/10.5194/acp-8-2213-2008</a>, 2008.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib52"><label>52</label><mixed-citation>
      
Sinha, V., Williams, J., Diesch, J. M., Drewnick, F., Martinez, M., Harder, H., Regelin, E., Kubistin, D., Bozem, H., Hosaynali-Beygi, Z., Fischer, H., Andrés-Hernández, M. D., Kartal, D., Adame, J. A., and Lelieveld, J.:
Constraints on instantaneous ozone production rates and regimes during DOMINO derived using in-situ OH reactivity measurements, Atmos. Chem. Phys., 12, 7269–7283, <a href="https://doi.org/10.5194/acp-12-7269-2012" target="_blank">https://doi.org/10.5194/acp-12-7269-2012</a>, 2012.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib53"><label>53</label><mixed-citation>
      
Song, B., Yan, X., Tan, S., Sai, B., Lai, S., Yu, H., Ou, C., and Lu, X.:
Human mobility models reveal the underlying mechanism of seasonal movements across China, Int. J. Mod. Phys. C, 33, 2250054, <a href="https://doi.org/10.1142/S0129183122500541" target="_blank">https://doi.org/10.1142/S0129183122500541</a>, 2022.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib54"><label>54</label><mixed-citation>
      
Stone, D., Whalley, L. K., and Heard, D. E.:
Tropospheric OH and HO<sub>2</sub> radicals: field measurements and model comparisons, Chem. Soc. Rev., 41, 6348–6404, <a href="https://doi.org/10.1039/c2cs35140d" target="_blank">https://doi.org/10.1039/c2cs35140d</a>, 2012.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib55"><label>55</label><mixed-citation>
      
Stone, D., Whalley, L. K., Ingham, T., Edwards, P. M., Cryer, D. R., Brumby, C. A., Seakins, P. W., and Heard, D. E.:
Measurement of OH reactivity by laser flash photolysis coupled with laser-induced fluorescence spectroscopy, Atmos. Meas. Tech., 9, 2827–2844, <a href="https://doi.org/10.5194/amt-9-2827-2016" target="_blank">https://doi.org/10.5194/amt-9-2827-2016</a>, 2016.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib56"><label>56</label><mixed-citation>
      
Teng, C. C., Yan, C., Rousso, A., Zhong, H., Chen, T., Zhang, E. J., Ju, Y., and Wysocki, G.:
Time-resolved HO<sub>2</sub> detection with Faraday rotation spectroscopy in a photolysis reactor, Opt. Express, 29, 2769–2779, <a href="https://doi.org/10.1364/OE.413063" target="_blank">https://doi.org/10.1364/OE.413063</a>, 2021.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib57"><label>57</label><mixed-citation>
      
Trutna, W. R. and Byer, R. L.:
Multiple-pass Raman gain cell, Appl. Optics, 19, 301–312, <a href="https://doi.org/10.1364/AO.19.000301" target="_blank">https://doi.org/10.1364/AO.19.000301</a>, 1980.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib58"><label>58</label><mixed-citation>
      
Wang, W., Li, X., Cheng, Y., Parrish, D. D., Ni, R., Tan, Z., Liu, Y., Lu, S., Wu, Y., Chen, S., Lu, K., Hu, M., Zeng, L., Shao, M., Huang, C., Tian, X., Leung, K. M., Chen, L., Fan, M., Zhang, Q., Rohrer, F., Wahner, A., Pöschl, U., Su, H., and Zhang, Y.:
Ozone pollution mitigation strategy informed by long-term trends of atmospheric oxidation capacity, Nat. Geosci., 17, 20–25, <a href="https://doi.org/10.1038/s41561-023-01334-9" target="_blank">https://doi.org/10.1038/s41561-023-01334-9</a>, 2023.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib59"><label>59</label><mixed-citation>
      
Wei, N., Fang, B., Zhao, W., Wang, C., Yang, N., Zhang, W., Chen, W., and Fittschen, C.:
Time-resolved laser-flash photolysis Faraday rotation spectrometer: a new tool for total OH reactivity measurement and free radical kinetics research, Anal. Chem., 92, 4334–4339, <a href="https://doi.org/10.1021/acs.analchem.9b05117" target="_blank">https://doi.org/10.1021/acs.analchem.9b05117</a>, 2020.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib60"><label>60</label><mixed-citation>
      
Wei, N., Zhao, W., Yao, Y., Wang, H., Liu, Z., Xu, X., Rahman, M., Zhang, C., Fittschen, C., and Zhang, W.:
Peroxy radical chemistry during ozone photochemical pollution season at a suburban site in the boundary of Jiangsu–Anhui–Shandong–Henan region, China, Sci. Total Environ., 904, 166355, <a href="https://doi.org/10.1016/j.scitotenv.2023.166355" target="_blank">https://doi.org/10.1016/j.scitotenv.2023.166355</a>, 2023.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib61"><label>61</label><mixed-citation>
      
Westberg, J. and Axner, O.:
Lineshape asymmetries in Faraday modulation spectroscopy, Appl. Phys. B, 116, 467–476, <a href="https://doi.org/10.1007/s00340-013-5721-x" target="_blank">https://doi.org/10.1007/s00340-013-5721-x</a>, 2014.


    </mixed-citation></ref-html>
<ref-html id="bib1.bib62"><label>62</label><mixed-citation>
      
Wolfe, G. M., Marvin, M. R., Roberts, S. J., Travis, K. R., and Liao, J.:
The Framework for 0-D Atmospheric Modeling (F0AM) v3.1, Geosci. Model Dev., 9, 3309–3319, <a href="https://doi.org/10.5194/gmd-9-3309-2016" target="_blank">https://doi.org/10.5194/gmd-9-3309-2016</a>, 2016.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib63"><label>63</label><mixed-citation>
      
Yan, C., Teng, C. C., Chen, T., Zhong, H., Rousso, A., Zhao, H., Ma, G., Wysocki, G., and Ju, Y.:
The kinetic study of excited singlet oxygen atom O(<sup>1</sup>D) reactions with acetylene, Combust. Flame, 212, 135–141, <a href="https://doi.org/10.1016/j.combustflame.2019.10.034" target="_blank">https://doi.org/10.1016/j.combustflame.2019.10.034</a>, 2020.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib64"><label>64</label><mixed-citation>
      
Yang, Y., Shao, M., Wang, X., Nölscher, A. C., Kessel, S., Guenther, A., and Williams, J.:
Towards a quantitative understanding of total OH reactivity: A review, Atmos. Environ., 134, 147–161, <a href="https://doi.org/10.1016/j.atmosenv.2016.03.010" target="_blank">https://doi.org/10.1016/j.atmosenv.2016.03.010</a>, 2016.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib65"><label>65</label><mixed-citation>
      
Yang, Y., Shao, M., Keßel, S., Li, Y., Lu, K., Lu, S., Williams, J., Zhang, Y., Zeng, L., Nölscher, A. C., Wu, Y., Wang, X., and Zheng, J.:
How the OH reactivity affects the ozone production efficiency: case studies in Beijing and Heshan, China, Atmos. Chem. Phys., 17, 7127–7142, <a href="https://doi.org/10.5194/acp-17-7127-2017" target="_blank">https://doi.org/10.5194/acp-17-7127-2017</a>, 2017.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib66"><label>66</label><mixed-citation>
      
Zannoni, N., Dusanter, S., Gros, V., Sarda Esteve, R., Michoud, V., Sinha, V., Locoge, N., and Bonsang, B.:
Intercomparison of two comparative reactivity method instruments inf the Mediterranean basin during summer 2013, Atmos. Meas. Tech., 8, 3851–3865, <a href="https://doi.org/10.5194/amt-8-3851-2015" target="_blank">https://doi.org/10.5194/amt-8-3851-2015</a>, 2015.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib67"><label>67</label><mixed-citation>
      
Zhao, W., Wysocki, G., Chen, W., Fertein, E., Coq, L. D., Petiprez, D., and Zhang, W.:
Sensitive and selective detection of OH radicals using Faraday rotation spectroscopy at 2.8&thinsp;µm, Opt. Express, 19, 2493–2501, <a href="https://doi.org/10.1364/OE.19.002493" target="_blank">https://doi.org/10.1364/OE.19.002493</a>, 2011.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib68"><label>68</label><mixed-citation>
      
Zhao, W., Wyscoki, G., Chen, W., Zhang, W.:
High sensitivity Faraday rotation spectrometer for hydroxyl radical detection at 2.8&thinsp;µm, Appl. Phys. B, 109, 511–519, <a href="https://doi.org/10.1007/s00340-012-5089-3" target="_blank">https://doi.org/10.1007/s00340-012-5089-3</a>, 2012.

    </mixed-citation></ref-html>
<ref-html id="bib1.bib69"><label>69</label><mixed-citation>
      
Zhao, W., Fang, B., Lin, X., Gai, Y., Zhang, W., Chen, W., Chen, Z., Zhang, H., and Chen, W.:
Superconducting-magnet-based Faraday rotation spectrometer for real time in situ measurement of OH radicals at 10<sup>6</sup>&thinsp;molecule∕cm<sup>3</sup> level in an atmospheric simulation chamber, Anal. Chem., 90, 3958–3964, <a href="https://doi.org/10.1021/acs.analchem.7b04949" target="_blank">https://doi.org/10.1021/acs.analchem.7b04949</a>, 2018.

    </mixed-citation></ref-html>--></article>
