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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>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-2-2259-2002</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>02</day>
<month>12</month>
<year>2002</year>
</pub-date>
<volume>2</volume>
<issue>6</issue>
<fpage>2259</fpage>
<lpage>2296</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/2/2259/2002/acpd-2-2259-2002.html">This article is available from http://www.atmos-chem-phys-discuss.net/2/2259/2002/acpd-2-2259-2002.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/2/2259/2002/acpd-2-2259-2002.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/2/2259/2002/acpd-2-2259-2002.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 April). 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 could be adapted to
      other mountainous measurement sites.</p>
</abstract>
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