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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-11-10331-2011</article-id>
<title-group>
<article-title>Evaluation of a three-dimensional chemical transport model (PMCAMx) in the European domain during the EUCAARI May 2008 campaign</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Fountoukis</surname>
<given-names>C.</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>Racherla</surname>
<given-names>P. N.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Denier van der Gon</surname>
<given-names>H. A. C.</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>Polymeneas</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Charalampidis</surname>
<given-names>P. E.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pilinis</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wiedensohler</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Dall&apos;Osto</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>O&apos;Dowd</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pandis</surname>
<given-names>S. N.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Chemical Engineering and High Temperature Chemical Processes, Foundation for Research and Technology Hellas (FORTH), Patras, Greece</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>NASA Goddard Institute for Space Studies, New York, NY 10025, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>TNO Built Environment and Geosciences, Princetonlaan 6, 3584 CB Utrecht, The Netherlands</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Environment, University of the Aegean, University Hill, 81100, Mytilene, Greece</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Leibniz Institute for Tropospheric Research, 04318 Leipzig, Germany</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>School of Physics and Centre for Climate &amp; Air Pollution Studies, National University of Ireland Galway, University Road, Galway, Ireland</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>Department of Chemical Engineering, University of Patras, Patras, Greece</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>Department of Chemical Engineering, Carnegie Mellon University, Pittsburgh, PA 15213, USA</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>now at: Institute for Environmental Assessment and Water Research (IDï¿½A-CSIC), Barcelona, Spain</addr-line>
</aff>
<pub-date pub-type="epub">
<day>18</day>
<month>10</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>20</issue>
<fpage>10331</fpage>
<lpage>10347</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/11/10331/2011/acp-11-10331-2011.html">This article is available from http://www.atmos-chem-phys.net/11/10331/2011/acp-11-10331-2011.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/10331/2011/acp-11-10331-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/10331/2011/acp-11-10331-2011.pdf</self-uri>
<abstract>
<p>PMCAMx-2008, a detailed three-dimensional chemical transport model (CTM),
was applied to Europe to simulate the mass concentration and chemical
composition of particulate matter (PM) during May 2008. The model includes a
state-of-the-art organic aerosol module which is based on the volatility
basis set framework treating both primary and secondary organic components
as semivolatile and photochemically reactive. The model performance is
evaluated against high time resolution aerosol mass spectrometer (AMS)
ground and airborne measurements. Overall, organic aerosol is predicted to
account for 32% of total PM&lt;sub&gt;1&lt;/sub&gt; at ground level during May 2008,
followed by sulfate (30%), crustal material and sea-salt (14%),
ammonium (13%), nitrate (7%), and elemental carbon (4%). The model
predicts that fresh primary OA (POA) is a small contributor to organic PM
concentrations in Europe during late spring, and that oxygenated species
(oxidized primary and biogenic secondary) dominate the ambient OA. The
Mediterranean region is the only area in Europe where sulfate concentrations
are predicted to be much higher than the OA, while organic matter is
predicted to be the dominant PM&lt;sub&gt;1&lt;/sub&gt; species in central and northern
Europe. The comparison of the model predictions with the ground measurements
in four measurement stations is encouraging. The model reproduces more than
94% of the daily averaged data and more than 87% of the hourly data
within a factor of 2 for PM&lt;sub&gt;1&lt;/sub&gt; OA. The model tends to predict relatively
flat diurnal profiles for PM&lt;sub&gt;1&lt;/sub&gt; OA in many areas, both rural and urban in
agreement with the available measurements. The model performance against the
high time resolution airborne measurements at multiple altitudes and
locations is as good as its performance against the ground level hourly
measurements. There is no evidence of missing sources of OA aloft over
Europe during this period.</p>
</abstract>
<counts><page-count count="17"/></counts>
</article-meta>
</front>
<body/>
<back>
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