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<front>
<journal-meta>
<journal-id journal-id-type="publisher">AMTD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Measurement Techniques Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">AMTD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Meas. Tech. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1867-8610</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/amtd-5-3079-2012</article-id>
<title-group>
<article-title>A Cavity-Enhanced Differential Optical Absorption Spectroscopy instrument for measurement of BrO, HCHO, HONO and O&lt;sub&gt;3&lt;/sub&gt;</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hoch</surname>
<given-names>D. J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Buxmann</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sihler</surname>
<given-names>H.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pöhler</surname>
<given-names>D.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zetzsch</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Platt</surname>
<given-names>U.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Environmental Physics, University of Heidelberg, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Max-Planck-Institute for Chemistry, Mainz, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Atmospheric Chemistry Research Laboratory, University of Bayreuth, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>26</day>
<month>04</month>
<year>2012</year>
</pub-date>
<volume>5</volume>
<issue>2</issue>
<fpage>3079</fpage>
<lpage>3115</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2012 D. J. Hoch et al.</copyright-statement>
<copyright-year>2012</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://amt.copernicus.org/preprints/5/3079/2012/amtd-5-3079-2012.html">This article is available from https://amt.copernicus.org/preprints/5/3079/2012/amtd-5-3079-2012.html</self-uri>
<self-uri xlink:href="https://amt.copernicus.org/preprints/5/3079/2012/amtd-5-3079-2012.pdf">The full text article is available as a PDF file from https://amt.copernicus.org/preprints/5/3079/2012/amtd-5-3079-2012.pdf</self-uri>
<abstract>
<p>The chemistry of the troposphere and specifically the global tropospheric
ozone budget is affected by reactive halogen compounds like BrO or ClO.
Bromine monoxide (BrO) plays an important role in the processes of ozone
destruction, disturbance of NO&lt;sub&gt;x&lt;/sub&gt; and HO&lt;sub&gt;x&lt;/sub&gt; chemistry, oxidation of DMS, and the
deposition of elementary mercury. In the troposphere BrO has been detected in
polar regions, at salt lakes, in volcanic plumes, and in the marine boundary
layer. For a better understanding of these processes instruments with high
spatial resolution and high sensitivity are necessary. A Cavity Enhanced
Differential Optical Absorption Spectroscopy (CE-DOAS) instrument was
designed and applied. For the first time, such an instrument uses an UV-LED
in the UV-wavelength range (325–365 nm) to identify BrO. In laboratory
studies at the Atmospheric Chemistry Research Laboratory, University of
Bayreuth, Germany, BrO, as well as HONO, HCHO, O&lt;sub&gt;3&lt;/sub&gt;, and O&lt;sub&gt;4&lt;/sub&gt;,
could be reliable determined at detection limits (for five minutes
integration time) of 20 ppt for BrO, 9.1 ppb for HCHO, 970 ppt for HONO,
and 91 ppb for O&lt;sub&gt;3&lt;/sub&gt;, respectively. The best detection limits for BrO
(11 ppt), HCHO (5.1 ppb), HONO (490 ppt), and O&lt;sub&gt;3&lt;/sub&gt; (59 ppb) were
achieved for integration times of 81 min or less.</p>
</abstract>
<counts><page-count count="37"/></counts>
</article-meta>
</front>
<body/>
<back>
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