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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys-discuss.net/inc/acpd/copernicus.dtd">
<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>1</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2001</publication_year>
	</journal>
	<doi>10.5194/acpd-1-411-2001</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/1/411/2001/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/1/411/2001/acpd-1-411-2001.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/1/411/2001/acpd-1-411-2001.pdf</fulltext_pdf>
	<start_page>411</start_page>
	<end_page>438</end_page>
	<publication_date>2001-12-13</publication_date>
	<article_title content_type="html">Tropospheric NO&lt;sub&gt;2&lt;/sub&gt; columns: a comparison between model and retrieved data from GOME measurements</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Lauer</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>M. Dameris</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>A. Richter</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>J. P. Burrows</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">DLR Institut für Physik der Atmosphäre, Oberpfaffenhofen, D-82234 Wessling, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Institut für Umweltphysik, Universität Bremen, D-28359 Bremen, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">Tropospheric
      NO&lt;sub&gt;2&lt;/sub&gt; plays a variety of significant roles in atmospheric chemistry. In the troposphere it is one of the most
      significant precursors of photochemical ozone (O&lt;sub&gt;3&lt;/sub&gt;)
      production and
      nitric acid (HNO&lt;sub&gt;3&lt;/sub&gt;). In this study tropospheric
      NO&lt;sub&gt;2&lt;/sub&gt;
      columns were calculated by the fully coupled chemistry-climate model ECHAM4.L39(DLR)/CHEM. These have been compared with tropospheric
      NO&lt;sub&gt;2&lt;/sub&gt; columns, retrieved using the tropospheric excess method
      from measurements by the Global Ozone Monitoring Experiment (GOME) of up-welling earthshine irradiance and the extraterrestrial
      radiance. GOME is part of the core payload of the second European Research Satellite (ERS-2). For this study the first five years of GOME
      measurements have been used. The period of five years of observational data is sufficient to enable a comparison based on
      climatological averages and with global coverage, focussing on the geographical distribution of the tropospheric
      NO&lt;sub&gt;2&lt;/sub&gt;, for the
      first time.
      A new approach of analysing regional differences (i.e. on continental
      scales) by calculating individual averages for different environments provides more detailed information about specific
      NO&lt;sub&gt;x&lt;/sub&gt; sources
      and of their seasonal variations. The results obtained enable the validity of the model
      NO&lt;sub&gt;2&lt;/sub&gt; source distribution and the
      assumptions used to separate tropospheric and stratospheric parts of the
      NO&lt;sub&gt;2&lt;/sub&gt; column amount from the satellite measurements to be
      investigated.</abstract>
	<references>
	</references>
</article>

