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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-8-4117-2008</article-id>
<title-group>
<article-title>Lagrangian transport modelling for CO&lt;sub&gt;2&lt;/sub&gt; using two different biosphere models</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pieterse</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Vermeulen</surname>
<given-names>A. T.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Baker</surname>
<given-names>I. T.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Denning</surname>
<given-names>A. S.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Energy research Centre of the Netherlands, Petten, The Netherlands</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute for Marine and Atmospheric Research Utrecht, Utrecht, The Netherlands</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Colorado State University, Fort Collins, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>28</day>
<month>02</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>1</issue>
<fpage>4117</fpage>
<lpage>4154</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2008 G. Pieterse et al.</copyright-statement>
<copyright-year>2008</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Generic License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by-nc-sa/2.5/">https://creativecommons.org/licenses/by-nc-sa/2.5/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://acp.copernicus.org/preprints/8/4117/2008/acpd-8-4117-2008.html">This article is available from https://acp.copernicus.org/preprints/8/4117/2008/acpd-8-4117-2008.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/preprints/8/4117/2008/acpd-8-4117-2008.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/preprints/8/4117/2008/acpd-8-4117-2008.pdf</self-uri>
<abstract>
<p>In this work, the performance of the Framework for Atmosphere-Canopy Exchange Modelling (FACEM: Pieterse et al., 2007) coupled
to a Lagrangian atmospheric transport model is evaluated for carbon dioxide. Before incorporating FACEM into the Lagrangian
COMET model (Vermeulen et al., 2006), its performance for the European domain is compared with the Simple
Biosphere model (SiB3: Sellers et al., 1996). Overall, FACEM is well correlated to SiB3 (&lt;i&gt;R&lt;sup&gt;2&lt;/sup&gt;&amp;ge;&lt;/i&gt;0.60),
 but shows less variability for regions with predominantly bare soil. There is no significant overall bias between
 the models except for the winter conditions and in general for the Iberian peninsula. When coupled to the COMET
 transport model, both biosphere models yield similar correlations (&lt;i&gt;R&lt;sup&gt;2&lt;/sup&gt;&amp;ge;&lt;/i&gt;0.60) and bias relative to
 the 1-hourly concentration measurements for the year 2002, performed at three different sites in Europe;
 Cabauw (Netherlands), Hegyhatsal (Hungary) and Mace Head (Ireland). The overall results indicate that
 FACEM is comparable to SiB3 in terms of its applicability for atmospheric modelling studies.</p>
</abstract>
<counts><page-count count="38"/></counts>
</article-meta>
</front>
<body/>
<back>
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