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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</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/acp-14-7601-2014</article-id>
<title-group>
<article-title>The fate of NO&lt;sub&gt;x&lt;/sub&gt; emissions due to nocturnal oxidation at high latitudes: 1-D simulations and sensitivity experiments</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Joyce</surname>
<given-names>P. L.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>von Glasow</surname>
<given-names>R.</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>Simpson</surname>
<given-names>W. R.</given-names>
<ext-link>https://orcid.org/0000-0002-8596-7290</ext-link>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Chemistry and Biochemistry, University of Alaska, Fairbanks, AK, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Geophysical Institute, University of Alaska, Fairbanks, AK, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, University of East Anglia, Norwich, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>29</day>
<month>07</month>
<year>2014</year>
</pub-date>
<volume>14</volume>
<issue>14</issue>
<fpage>7601</fpage>
<lpage>7616</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2014 P. L. Joyce et al.</copyright-statement>
<copyright-year>2014</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://acp.copernicus.org/articles/14/7601/2014/acp-14-7601-2014.html">This article is available from https://acp.copernicus.org/articles/14/7601/2014/acp-14-7601-2014.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/14/7601/2014/acp-14-7601-2014.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/14/7601/2014/acp-14-7601-2014.pdf</self-uri>
<abstract>
<p>The fate of nitrogen oxide pollution during high-latitude winter is controlled by reactions of
  dinitrogen pentoxide (N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;) and is highly affected by the competition between
  heterogeneous atmospheric reactions and deposition to the snowpack. MISTRA (MIcrophysical STRAtus), a 1-D photochemical
  model, simulated an urban pollution plume from Fairbanks, Alaska to investigate this competition
  of N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; reactions and explore sensitivity to model parameters. It was found that dry
  deposition of N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; made up a significant fraction of N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; loss near the
  snowpack, but reactions on aerosol particles dominated loss of N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; over the integrated
  atmospheric column. Sensitivity experiments found the fate of NO&lt;sub&gt;x&lt;/sub&gt; emissions were most
  sensitive to NO  emission flux, photolysis rates, and ambient temperature. The results
  indicate a strong sensitivity to urban area density, season and clouds, and temperature, implying
  a strong sensitivity of the results to urban planning and climate change. Results suggest that
  secondary formation of particulate (PM&lt;sub&gt;2.5&lt;/sub&gt;) nitrate in the Fairbanks downtown area does
  not contribute significant mass to the total PM&lt;sub&gt;2.5&lt;/sub&gt; concentration, but appreciable
  amounts are formed downwind of downtown due to nocturnal NO&lt;sub&gt;x&lt;/sub&gt; oxidation and subsequent
  reaction with ammonia on aerosol particles.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
<body/>
<back>
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