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<article language="en">
	<journal>
		<journal_title>Geoscientific Model Development Discussions</journal_title>
		<journal_url>www.geosci-model-dev-discuss.net</journal_url>
		<issn>1991-9611</issn>
		<eissn>1991-962X</eissn>
		<volume_number>3</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/gmdd-3-391-2010</doi>
	<article_url>http://www.geosci-model-dev-discuss.net/3/391/2010/</article_url>
	<abstract_html>http://www.geosci-model-dev-discuss.net/3/391/2010/gmdd-3-391-2010.html</abstract_html>
	<fulltext_pdf>http://www.geosci-model-dev-discuss.net/3/391/2010/gmdd-3-391-2010.pdf</fulltext_pdf>
	<start_page>391</start_page>
	<end_page>449</end_page>
	<publication_date>2010-04-08</publication_date>
	<article_title content_type="html">Current status of the ability of the GEMS/MACC models to reproduce the tropospheric CO vertical distribution as measured by MOZAIC</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>N. Elguindi</name>
			<email>soln@aero.obs-mis.fr</email>
		</author>
		<author numeration="2" affiliations="1,2,3">
			<name>C. OrdÃ³Ã±ez</name>
		</author>
		<author numeration="3" affiliations="1,2">
			<name>V. Thouret</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>J. Flemming</name>
		</author>
		<author numeration="5" affiliations="5">
			<name>O. Stein</name>
		</author>
		<author numeration="6" affiliations="6">
			<name>V. Huijnen</name>
		</author>
		<author numeration="7" affiliations="7">
			<name>P. Moinat</name>
		</author>
		<author numeration="8" affiliations="4">
			<name>A. Inness</name>
		</author>
		<author numeration="9" affiliations="7">
			<name>V.-H. Peuch</name>
		</author>
		<author numeration="10" affiliations="8">
			<name>A. Stohl</name>
		</author>
		<author numeration="11" affiliations="9">
			<name>S. Turquety</name>
		</author>
		<author numeration="12" affiliations="1,2">
			<name>J.-P. Cammas</name>
		</author>
		<author numeration="13" affiliations="5">
			<name>M. Schultz</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">UniversitÃ© de Toulouse, UPS, LA (Laboratoire d&apos;AÃ©rologie), 14 avenue Edouard Belin, Toulouse, France</affiliation>
		<affiliation numeration="2" content_type="html">CNRS, LA (Laboratoire d&apos;AÃ©rologie), UMR 5560, 31400 Toulouse, France</affiliation>
		<affiliation numeration="3" content_type="html">Met Office, Atmospheric Dispersion Group, Exeter, UK</affiliation>
		<affiliation numeration="4" content_type="html">European Centre for Medium-Range Weather Forecasts (ECMWF), Reading, UK</affiliation>
		<affiliation numeration="5" content_type="html">FZ JÃ¼lich, Institute for Chemistry and Dynamics of the Geosphere-Troposphere, JÃ¼lich, Germany</affiliation>
		<affiliation numeration="6" content_type="html">Royal Netherlands Meteorological Institute (KNMI), De Bilt, The Netherlands</affiliation>
		<affiliation numeration="7" content_type="html">MÃ©tÃ©o France, Centre National de Recherches MÃ©tÃ©orologiques, Toulouse, France</affiliation>
		<affiliation numeration="8" content_type="html">Norwegian Institute for Air Research, Kjeller, Norway</affiliation>
		<affiliation numeration="9" content_type="html">Laboratoire de MÃ©tÃ©orologie Dynamique/IPSL, UPMC Univ. Paris 06, Paris, France</affiliation>
	</affiliations>
	<abstract content_type="html">Vertical profiles of CO taken from the MOZAIC aircraft database are used to
present (1) a global analysis of CO seasonal averages and interannual
variability for the years 2002â€“2007 and (2) a global validation of CO
estimates produced by the MACC models for 2004, including an assessment of
their ability to transport pollutants originating from the Alaskan/Canadian
wildfires. Seasonal averages and interannual variability from several MOZAIC
sites representing different regions of the world show that CO concentrations
are highest and most variable during the winter season. The inter-regional
variability is significant with concentrations increasing eastward from
Europe to Japan. The impact of the intense boreal fires, particularly in
Russia, during the fall of 2002 on the Northern Hemisphere CO concentrations
throughout the troposphere is well represented by the MOZAIC data.


&lt;br&gt;&lt;br&gt;

A global validation of the GEMS/MACC GRG models which include three
stand-alone CTMs (MOZART, MOCAGE and TM5) and the coupled ECMWF Integrated
Forecasting System (IFS)/MOZART model with and without MOPITT CO data
assimilation show that the models have a tendency to underestimate CO. The
models perform best in Europe and the US where biases range from 0 to â€“25%
in the free troposphere and from 0 to â€“50% in the surface and boundary
layers (BL). The biases are largest in the winter and during the daytime when
emissions are highest, indicating that current inventories are too low. Data
assimilation is shown to reduce biases by up to 25% in some regions. The
models are not able to reproduce well the CO plumes originating from the
Alaskan/Canadian wildfires at downwind locations in the eastern US and
Europe, not even with assimilation. Sensitivity tests reveal that this is
mainly due to deficiencies in the fire emissions inventory and injection
height.</abstract>
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</article>

