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<article language="en">
	<journal>
		<journal_title>Biogeosciences</journal_title>
		<journal_url>www.biogeosciences.net</journal_url>
		<issn>1726-4170</issn>
		<eissn>1726-4189</eissn>
		<volume_number>6</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/bg-6-633-2009</doi>
	<article_url>http://www.biogeosciences.net/6/633/2009/</article_url>
	<abstract_html>http://www.biogeosciences.net/6/633/2009/bg-6-633-2009.html</abstract_html>
	<fulltext_pdf>http://www.biogeosciences.net/6/633/2009/bg-6-633-2009.pdf</fulltext_pdf>
	<start_page>633</start_page>
	<end_page>646</end_page>
	<publication_date>2009-04-23</publication_date>
	<article_title content_type="html">Mesoscale modelling of the CO&lt;sub&gt;2&lt;/sub&gt; interactions between the surface and the atmosphere applied to the April 2007 CERES field experiment</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>C. Sarrat</name>
			<email>claire.sarrat@cnrm.meteo.fr</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. Noilhan</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>P. Lacarrère</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>E. Ceschia</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>P. Ciais</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>A. J. Dolman</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>J. A. Elbers</name>
		</author>
		<author numeration="8" affiliations="6">
			<name>C. Gerbig</name>
		</author>
		<author numeration="9" affiliations="7">
			<name>B. Gioli</name>
		</author>
		<author numeration="10" affiliations="3">
			<name>T. Lauvaux</name>
		</author>
		<author numeration="11" affiliations="7">
			<name>F. Miglietta</name>
		</author>
		<author numeration="12" affiliations="8">
			<name>B. Neininger</name>
		</author>
		<author numeration="13" affiliations="3">
			<name>M. Ramonet</name>
		</author>
		<author numeration="14" affiliations="5">
			<name>O. Vellinga</name>
		</author>
		<author numeration="15" affiliations="9">
			<name>J. M. Bonnefond</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">CNRM-GAME, Météo France, 42 avenue Coriolis, 31057 Toulouse, France</affiliation>
		<affiliation numeration="2" content_type="html">Vrije University, De Boelelaan 1085,1081 HV Amsterdam, The Netherlands</affiliation>
		<affiliation numeration="3" content_type="html">Max Planck Institute for Biogeochemistry, Hans-Knoell-Str. 10, 07745 Jena, Germany</affiliation>
		<affiliation numeration="4" content_type="html">ALTERRA, Droevendaalsesteeg 3, 6708 PB Wageningen, The Netherlands</affiliation>
		<affiliation numeration="5" content_type="html">Ibimet CNR, Via Giovanni Caproni 8, 50145 Firenze, Italy</affiliation>
		<affiliation numeration="6" content_type="html">MetAir, Sonnenberg 27, 6313 Menzingen, Switzerland</affiliation>
		<affiliation numeration="7" content_type="html">LSCE, CEA/Saclay, 91191 Gif-sur-Yvette, France</affiliation>
		<affiliation numeration="8" content_type="html">CESBIO, 8 av. E. Belin, 31401 Toulouse, France</affiliation>
		<affiliation numeration="9" content_type="html">INRA, B.P. 81, 33883 Villenave d&apos;Ornon, France</affiliation>
	</affiliations>
	<abstract content_type="html">This paper describes a numerical interpretation of the April 2007, CarboEurope
Regional Experiment Strategy (CERES) campaign, devoted to the study of the
CO&lt;sub&gt;2&lt;/sub&gt; cycle at the regional scale. Four consecutive clear sky days with
intensive observations of CO&lt;sub&gt;2&lt;/sub&gt; concentration, fluxes at the surface and
in the boundary layer have been simulated with the Meso-NH mesoscale model,
coupled to ISBA-A-gs land surface model. The main result of this paper is to
show how aircraft observations of CO&lt;sub&gt;2&lt;/sub&gt; concentration have been used to
identify surface model errors and to calibrate the CO&lt;sub&gt;2&lt;/sub&gt; driving component of the surface model.
In fact, the comparisons between modelled and observed CO&lt;sub&gt;2&lt;/sub&gt; concentrations
within the Atmospheric Boundary Layer (ABL) allow to calibrate and correct
not only the parameterization of respired CO&lt;sub&gt;2&lt;/sub&gt; fluxes by the ecosystem
but also the Leaf Area Index (LAI) of the dominating land cover.
After this calibration, the paper describes systematic comparisons of the
model outputs with numerous data collected during the CERES campaign, in
April 2007. For instance, the originality of this paper is the spatial
integration of the comparisons. In fact, the aircraft observations of
CO&lt;sub&gt;2&lt;/sub&gt; concentration and fluxes and energy fluxes are used for the model
validation from the local to the regional scale. As a conclusion, the
CO&lt;sub&gt;2&lt;/sub&gt; budgeting approach from the mesoscale model shows that the winter
croplands are assimilating more CO&lt;sub&gt;2&lt;/sub&gt; than the pine forest, at this
stage of the year and this case study.</abstract>
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</article>

