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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>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-3-779-2003</article-id>
<title-group>
<article-title>Partitioning of reactive nitrogen (NO&lt;sub&gt;y&lt;/sub&gt;) and dependence on meteorological conditions in the lower free troposphere</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Zellweger</surname>
<given-names>C.</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>Forrer</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>Hofer</surname>
<given-names>P.</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>Nyeki</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</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>Schwarzenbach</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>Weingartner</surname>
<given-names>E.</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>Ammann</surname>
<given-names>M.</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>Baltensperger</surname>
<given-names>U.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>EMPA, CH-8600 Dübendorf, Switzerland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Paul Scherrer Institute, CH-5232 Villigen PSI, Switzerland</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Now at University of Zürich, CH-8057 Zürich, Switzerland</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Institute for Environmental Research, University of Essex, Colchester, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>19</day>
<month>06</month>
<year>2003</year>
</pub-date>
<volume>3</volume>
<issue>3</issue>
<fpage>779</fpage>
<lpage>796</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.net/3/779/2003/acp-3-779-2003.html">This article is available from http://www.atmos-chem-phys.net/3/779/2003/acp-3-779-2003.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/3/779/2003/acp-3-779-2003.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/3/779/2003/acp-3-779-2003.pdf</self-uri>
<abstract>
<p>Results of continuous nitrogen oxide (NO), nitrogen dioxide
      (NO&lt;sub&gt;2&lt;/sub&gt;), peroxyacetyl nitrate (PAN) and total reactive nitrogen (NO&lt;sub&gt;y&lt;/sub&gt;) measurements along with seasonal field campaigns
      of nitric acid (HNO&lt;sub&gt;3&lt;/sub&gt;) and particulate nitrate (NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;-&lt;/sup&gt;)
      measurements are presented for a two-year period at the high-alpine research station Jungfraujoch
      (JFJ), 3580 m asl. The NO&lt;sub&gt;y&lt;/sub&gt; mixing ratio and partitioning is shown to strongly
      depend on meteorological conditions. Knowledge of these meteorological transport processes allows discrimination between
      undisturbed (i.e. clean) and disturbed (i.e. influenced by regional pollution sources) free tropospheric (FT) conditions at
      the JFJ. Median NO&lt;sub&gt;y&lt;/sub&gt; concentrations during undisturbed FT periods ranged from
      350 pptv (winter, December to February) to 581 pptv (spring, March to May). PAN was found to be the
      dominant NO&lt;sub&gt;y&lt;/sub&gt; species during spring and summer, whereas NO&lt;sub&gt;2&lt;/sub&gt; was most abundant during autumn and winter. Particulate
      nitrate was found to contribute significantly to total NO&lt;sub&gt;y&lt;/sub&gt; during thermally induced vertical transport.
      Föhn events, synoptical lifting (e.g. fronts) and thermally induced vertical
      transport resulted in mixing ratios up to 10 times higher at the JFJ compared to undisturbed FT conditions. Furthermore this
      meteorological variability of the NO&lt;sub&gt;y&lt;/sub&gt; concentration and partitioning often dominated the seasonal variability. As a
      consequence the use of filters at the JFJ (and other mountainous sites) is crucial for the interpretation of data from such
      measurement sites. This study presents a further development of meteorological filters for the high-alpine site
      Jungfraujoch, which also could be modified and adapted to other mountainous
      measurement sites.</p>
</abstract>
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