<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "https://jats.nlm.nih.gov/nlm-dtd/publishing/3.0/journalpublishing3.dtd">
<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" article-type="research-article" specific-use="SMUR" dtd-version="3.0" xml:lang="en">
<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/amt-2018-21</article-id>
<title-group>
<article-title>IASI nitrous oxide (N&lt;sub&gt;2&lt;/sub&gt;O) retrievals: validation and application to
transport studies at daily time scales</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kangah</surname>
<given-names>Yannick</given-names>
<ext-link>https://orcid.org/0000-0003-2580-717X</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ricaud</surname>
<given-names>Philippe</given-names>
<ext-link>https://orcid.org/0000-0002-7133-1734</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Attié</surname>
<given-names>Jean-Luc</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Saitoh</surname>
<given-names>Naoko</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>Vidot</surname>
<given-names>Jérôme</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Brunel</surname>
<given-names>Pascal</given-names>
<ext-link>https://orcid.org/0000-0002-4546-228X</ext-link>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Quesada-Ruiz</surname>
<given-names>Samuel</given-names>
<ext-link>https://orcid.org/0000-0001-6508-1102</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>CNRM-GAME, Météo-France/CNRS UMR 3589, Toulouse, France</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Université de Toulouse, Laboratoire d’Aérologie, CNRS UMR 5560, Toulouse, France</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Center for Environmental Remote Sensing, Chiba University, Japan</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Centre de Météorologie Spatiale,DP/Météo-France, Lannion, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>13</day>
<month>04</month>
<year>2018</year>
</pub-date>
<volume>2018</volume>
<fpage>1</fpage>
<lpage>34</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2018 Yannick Kangah et al.</copyright-statement>
<copyright-year>2018</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/preprints/amt-2018-21/">This article is available from https://amt.copernicus.org/preprints/amt-2018-21/</self-uri>
<self-uri xlink:href="https://amt.copernicus.org/preprints/amt-2018-21/amt-2018-21.pdf">The full text article is available as a PDF file from https://amt.copernicus.org/preprints/amt-2018-21/amt-2018-21.pdf</self-uri>
<abstract>
<p>The aim of this paper is to present a method to retrieve nitrous oxide (N&lt;sub&gt;2&lt;/sub&gt;O) vertical profiles from the Infrared Atmospheric Sounding Interferometer (IASI) onboard the MetOp platform. We retrieved N&lt;sub&gt;2&lt;/sub&gt;O profiles using IASI clear sky radiances in 2 spectral bands: B1 and B2 centered at ∼&amp;thinsp;1280&amp;thinsp;cm&lt;sup&gt;&amp;minus;1&lt;/sup&gt; and ∼&amp;thinsp;2220&amp;thinsp;cm&lt;sup&gt;&amp;minus;1&lt;/sup&gt;, respectively. Both retrievals in B1
and B2 (hereafter referred to as N&lt;sub&gt;2&lt;/sub&gt;O_B1 and N&lt;sub&gt;2&lt;/sub&gt;O_B2, respectively) are sensitive to the mid-to-upper troposphere with a maximum of sensitivity at around 309&amp;thinsp;hPa. The degrees of freedom for N&lt;sub&gt;2&lt;/sub&gt;O_B1 and N&lt;sub&gt;2&lt;/sub&gt;O_B2 are 1.38 and 0.93, respectively. We validated the retrievals using the High-performance Instrumented Airborne Platform for Environmental Research Pole-to-Pole Observations (HIPPO). The comparisons between HIPPO and the two retrieved datasets show relatively low standard deviation errors around 1.5&amp;thinsp;% (∼&amp;thinsp;4.8&amp;thinsp;ppbv) and 1.0&amp;thinsp;% (∼&amp;thinsp;3.2&amp;thinsp;ppbv) for N&lt;sub&gt;2&lt;/sub&gt;O_B1 and N&lt;sub&gt;2&lt;/sub&gt;O_B2, respectively. However, the impact of H&lt;sub&gt;2&lt;/sub&gt;O contamination on N&lt;sub&gt;2&lt;/sub&gt;O_B1 due to its strong absorption bands in B1 significantly degrades the quality of the retrievals in
tropical regions. We analysed the scientific consistency of the retrievals at 309&amp;thinsp;hPa with a focus on the long-range transport of N&lt;sub&gt;2&lt;/sub&gt;O especially during the Asian summer monsoon. Over the mid-latitude regions, both variations of N&lt;sub&gt;2&lt;/sub&gt;O_B1 and N&lt;sub&gt;2&lt;/sub&gt;O_B2 at 309&amp;thinsp;hPa are influenced by the stratospheric N&lt;sub&gt;2&lt;/sub&gt;O-depleted air because of the relative coarse shape of the averaging kernel. The
analysis of N&lt;sub&gt;2&lt;/sub&gt;O_B2 using results from backtrajectories exhibits the capacity of these retrievals to capture long-range transport of air masses from Asia to northern Africa via the summer monsoon anticyclone on a daily basis. Thus, N&lt;sub&gt;2&lt;/sub&gt;O_B1 and N&lt;sub&gt;2&lt;/sub&gt;O_B2 offer an unprecedented possibility to study global upper tropospheric N&lt;sub&gt;2&lt;/sub&gt;O on a daily basis.</p>
</abstract>
<counts><page-count count="34"/></counts>
</article-meta>
</front>
<body/>
<back>
</back>
</article>