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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>2</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2002</publication_year>
	</journal>
	<doi>10.5194/acpd-2-2259-2002</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/2/2259/2002/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/2/2259/2002/acpd-2-2259-2002.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/2/2259/2002/acpd-2-2259-2002.pdf</fulltext_pdf>
	<start_page>2259</start_page>
	<end_page>2296</end_page>
	<publication_date>2002-12-02</publication_date>
	<article_title content_type="html">Partitioning of reactive nitrogen (NO&lt;sub&gt;y&lt;/sub&gt;) and dependence on meteorological conditions in the lower free troposphere</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>C. Zellweger</name>
		</author>
		<author numeration="2" affiliations="1,3">
			<name>J. Forrer</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>P. Hofer</name>
		</author>
		<author numeration="4" affiliations="2,4">
			<name>S. Nyeki</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>B. Schwarzenbach</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>E. Weingartner</name>
		</author>
		<author numeration="7" affiliations="2">
			<name>M. Ammann</name>
		</author>
		<author numeration="8" affiliations="2">
			<name>U. Baltensperger</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">EMPA, CH-8600 Dübendorf, Switzerland</affiliation>
		<affiliation numeration="2" content_type="html">Paul Scherrer Institute, CH-5232 Villigen PSI, Switzerland</affiliation>
		<affiliation numeration="3" content_type="html">Now at University of Zürich, CH-8057 Zürich, Switzerland</affiliation>
		<affiliation numeration="4" content_type="html">Institute for Environmental Research, University of Essex, Colchester, UK</affiliation>
	</affiliations>
	<abstract content_type="html">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.</abstract>
	<references>
	</references>
</article>

