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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>
</journal-title-group>
<issn pub-type="epub">1680-7324</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/acp-10-2795-2010</article-id>
<title-group>
<article-title>Nocturnal nitrogen oxides at a rural mountain-site in south-western Germany</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Crowley</surname>
<given-names>J. N.</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>Schuster</surname>
<given-names>G.</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>Pouvesle</surname>
<given-names>N.</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>Parchatka</surname>
<given-names>U.</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>Fischer</surname>
<given-names>H.</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>Bonn</surname>
<given-names>B.</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>Bingemer</surname>
<given-names>H.</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>Lelieveld</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Max-Planck-Institut fÃ¼r Chemie, Atmospheric Chemistry Dept., Mainz, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>UniversitÃ¤t Frankfurt, Fachbereich Geowissenschaften, Frankfurt am Main, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>25</day>
<month>03</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>6</issue>
<fpage>2795</fpage>
<lpage>2812</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>
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<self-uri xlink:href="http://www.atmos-chem-phys.net/10/2795/2010/acp-10-2795-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/2795/2010/acp-10-2795-2010.pdf</self-uri>
<abstract>
<p>A new, two-channel instrument for simultaneous NO&lt;sub&gt;3&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;
monitoring was used to make the first comprehensive set of nocturnal NO&lt;sub&gt;x&lt;/sub&gt;
measurements (NO, NO&lt;sub&gt;2&lt;/sub&gt;, NO&lt;sub&gt;3&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;) at the Taunus
Observatory, a rural mountain site (Kleiner Feldberg) in South-western
Germany. In May 2008, NO&lt;sub&gt;3&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; mixing ratios were well
above the instrumental detection limit (a few ppt) on all nights of the
campaign and were characterised by large variability. The concentrations of
NO&lt;sub&gt;3&lt;/sub&gt;, N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; and NO&lt;sub&gt;2&lt;/sub&gt; were consistent with the equilibrium
constant, &lt;I&gt;K&lt;/I&gt;&lt;sub&gt;2&lt;/sub&gt;, defining the rates of formation and thermal dissociation
of N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;. A steady-state lifetime analysis is consistent with the
loss of nocturnal NO&lt;sub&gt;x&lt;/sub&gt; being dominated by the reaction of NO&lt;sub&gt;3&lt;/sub&gt; with
volatile organic compounds in this forested region, with N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;
uptake to aerosols of secondary importance. Analysis of a limited dataset
obtained at high relative humidity indicated that the loss of N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;
by reaction with water vapour is less efficient (&amp;gt;factor 3) than derived
using laboratory kinetic data. The fraction of NO&lt;sub&gt;x&lt;/sub&gt; present as NO&lt;sub&gt;3&lt;/sub&gt; and
N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; reached ~20% on some nights, with night-time
losses of NO&lt;sub&gt;x&lt;/sub&gt; competing with daytime losses.</p>
</abstract>
<counts><page-count count="18"/></counts>
</article-meta>
</front>
<body/>
<back>
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