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<!DOCTYPE article SYSTEM "http://www.atmos-chem-phys.net/inc/acp/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>5</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acp-5-169-2005</doi>
	<article_url>http://www.atmos-chem-phys.net/5/169/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/5/169/2005/acp-5-169-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/5/169/2005/acp-5-169-2005.pdf</fulltext_pdf>
	<start_page>169</start_page>
	<end_page>190</end_page>
	<publication_date>2005-01-24</publication_date>
	<article_title content_type="html">Comparison and evaluation of modelled and GOME measurement derived tropospheric NO&lt;sub&gt;2&lt;/sub&gt; columns over Western and Eastern Europe</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>I. B. Konovalov</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>M. Beekmann</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>R. Vautard</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>J. P. Burrows</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>A. Richter</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>H. Nüß</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>N. Elansky</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Applied Physics, Russian Academy of Sciences, Nizhniy Novgorod, Russia</affiliation>
		<affiliation numeration="2" content_type="html">Service d’Aéronomie, Institut Pierre Simon Laplace, Paris, France</affiliation>
		<affiliation numeration="3" content_type="html">Laboratoire de Météorologie Dynamique, Institut Pierre Simon Laplace, Paris, France</affiliation>
		<affiliation numeration="4" content_type="html">Institute of Environmental Physics and Remote Sensing, IUP/IFE, University of Bremen, Bremen, Germany</affiliation>
		<affiliation numeration="5" content_type="html">Institute of Atmospheric Physics, Russian Academy of Sciences, Moscow, Russia</affiliation>
	</affiliations>
	<abstract content_type="html">We present the results of a first comparison of the tropospheric NO&lt;sub&gt;2&lt;/sub&gt; column amounts derived from the measurements of the Global Ozone Monitoring
Experiment (GOME) with the simulated data from a European scale chemistry
transport model (CTM) which is distinct from existing global scale CTMs in
higher horizontal resolution and more detailed description of the boundary
layer processes and emissions. We employ, on the one hand, the newly
developed extended version of the CHIMERE CTM, which covers both Western and
Eastern Europe, and, on the other hand, the most recent version (Version 2)
of GOME measurement based data-products, developed at the University of
Bremen. We evaluate our model with the data from ground based monitoring of
ozone and verify that it has a sufficiently high level of performance, which
is expected for a state-of-the-art continental scale CTM. The major focus of
the study is on a systematic statistical analysis and a comparison of
spatial variability of the tropospheric NO&lt;sub&gt;2&lt;/sub&gt; columns simulated with
CHIMERE and derived from GOME measurements. The analysis is performed
separately for Western and Eastern Europe using the data for summer months
of 1997 and 2001. In this way, we obtain useful information on the nature
and magnitudes of uncertainties of spatial distributions of the considered
data. Specifically, for Western Europe, it is found that the uncertainties
of NO&lt;sub&gt;2&lt;/sub&gt; columns from GOME and CHIMERE are predominantly of the
multiplicative character, and that the mean relative random (multiplicative)
errors of the GOME measurement derived and simulated data averaged over the
summer seasons considered do not exceed 23% and 32%, respectively. The
mean absolute (additive) errors of both kinds of the data are estimated to
be less than 3x10&lt;sup&gt;14&lt;/sup&gt;mol/cm&lt;sup&gt;2&lt;/sup&gt;. In Eastern Europe, the
uncertainties have more complex character, and the separation between their
multiplicative and additive parts is not sufficiently unambiguous. It is
found, however, that the total random errors of NO&lt;sub&gt;2&lt;/sub&gt; columns from both
GOME and CHIMERE over Eastern Europe are not, on the average, larger than
the errors of the NO&lt;sub&gt;2&lt;/sub&gt; columns with similar magnitudes over Western
Europe.</abstract>
	<references>
	</references>
</article>

