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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-9-183-2009</article-id>
<title-group>
<article-title>Observations of high rates of NO&lt;sub&gt;2&lt;/sub&gt; â€“ HONO conversion in the  nocturnal atmospheric boundary layer in Kathmandu, Nepal</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Yu</surname>
<given-names>Y.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Galle</surname>
<given-names>B.</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>Hodson</surname>
<given-names>E.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Panday</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Prinn</surname>
<given-names>R.</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>Wang</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Optical Remote Sensing, Radio and Space Science, Chalmers University, 41296  Gothenburg, Sweden</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts  Institute of Technology, Cambridge, MA 02139, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Jet Propulsion Laboratory, Pasadena, CA 91109, USA</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>now at: Department of Chemistry, UC Irvine, Irvine, CA 92697-2025, USA</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>now at: Ecological Process Modelling Unit, Swiss Federal Institute for Forest, Snow and Landscape Research, Birmensdorf, 8903, Switzerland</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>now at: Atmospheric and Oceanic program, Princeton University, Princeton, NJ  08544, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>06</day>
<month>01</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>1</issue>
<fpage>183</fpage>
<lpage>223</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/9/183/2009/acpd-9-183-2009.html">This article is available from http://www.atmos-chem-phys-discuss.net/9/183/2009/acpd-9-183-2009.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/9/183/2009/acpd-9-183-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/9/183/2009/acpd-9-183-2009.pdf</self-uri>
<abstract>
<p>Nitrous acid (HONO) plays a significant role in the atmosphere,
      especially in the polluted troposphere. Its photolysis after sunrise
      is an important source of hydroxyl free radicals (OH). Measurements of
      nitrous acid and other pollutants were carried out in the Kathmandu
      urban atmosphere during Januaryâ€“February 2003, contributing to the
      sparse knowledge of nitrous acid in South Asia. The results showed
      average nocturnal levels of HONO (1.7&amp;plusmn;0.8 ppbv),
      NO&lt;sub&gt;2&lt;/sub&gt; (17.9&amp;plusmn;10.2 ppbv), and PM&lt;sub&gt;10&lt;/sub&gt; (0.18&amp;plusmn&lt;/sub&gt;0.11 mg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;) in urban air in Kathmandu. Surprisingly high
      ratios of chemically formed secondary [HONO] to [NO&lt;sub&gt;2&lt;/sub&gt;] (up to
      30%) were found, which indicates unexpectedly efficient chemical
      conversion of NO&lt;sub&gt;2&lt;/sub&gt; to HONO in Kathmandu. The ratios of
      [HONO]/[NO&lt;sub&gt;2&lt;/sub&gt;] at nights are much higher than previously
      reported values from measurements in urban air in Europe, North
      America and Asia. The influence of aerosol plumes, relative humidity,
      aerosol surface and ground reactive surface, temperature on
      NO&lt;sub&gt;2&lt;/sub&gt;-HONO chemical conversion were discussed. The high
      humidity, strong and low inversion layer at night, and serious aerosol
      pollution burden may explain the particularly efficient conversion of
      NO&lt;sub&gt;2&lt;/sub&gt; to HONO.</p>
</abstract>
<counts><page-count count="41"/></counts>
</article-meta>
</front>
<body/>
<back>
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