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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-8-6587-2008</article-id>
<title-group>
<article-title>Modelling representation errors of atmospheric CO&lt;sub&gt;2&lt;/sub&gt; mixing ratios at a regional scale</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Tolk</surname>
<given-names>L. F.</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>Meesters</surname>
<given-names>A. G. C. A.</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>Dolman</surname>
<given-names>A. J.</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>Peters</surname>
<given-names>W.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>VU University Amsterdam, Amsterdam, The Netherlands</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Wageningen University and Research Centre, Wageningen, The Netherlands</addr-line>
</aff>
<pub-date pub-type="epub">
<day>17</day>
<month>11</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>22</issue>
<fpage>6587</fpage>
<lpage>6596</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<self-uri xlink:href="http://www.atmos-chem-phys.net/8/6587/2008/acp-8-6587-2008.html">This article is available from http://www.atmos-chem-phys.net/8/6587/2008/acp-8-6587-2008.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/8/6587/2008/acp-8-6587-2008.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/8/6587/2008/acp-8-6587-2008.pdf</self-uri>
<abstract>
<p>Inverse modelling of carbon sources and sinks requires an accurate quality
estimate of the modelling framework to obtain a realistic estimate of the
inferred fluxes and their uncertainties. So-called &quot;representation errors&quot;
result from our inability to correctly represent point observations with
simulated average values of model grid cells. They may add substantial
uncertainty to the interpretation of atmospheric CO&lt;sub&gt;2&lt;/sub&gt; mixing ratio data.
We simulated detailed variations in the CO&lt;sub&gt;2&lt;/sub&gt; mixing ratios with a high
resolution (2 km) mesoscale model (RAMS) to estimate the representation
errors introduced at larger model grid sizes of 10â€“100 km. We found that
meteorology is the main driver of representation errors in our study causing
spatial and temporal variations in the error estimate. Within the nocturnal
boundary layer, the representation errors are relatively large and mainly
caused by unresolved topography at lower model resolutions. During the day,
convective structures, mesoscale circulations, and surface CO&lt;sub&gt;2&lt;/sub&gt; flux
variability were found to be the main sources of representation errors.
Interpreting observations near a mesoscale circulation as representative for
air with the correct footprint relative to the front can reduce the
representation error substantially. The remaining representation error is
0.5â€“1.5 ppm at 20â€“100 km resolution.</p>
</abstract>
<counts><page-count count="10"/></counts>
</article-meta>
</front>
<body/>
<back>
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