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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>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-10-6645-2010</article-id>
<title-group>
<article-title>Modeling the regional impact of ship emissions on NO&lt;sub&gt;x&lt;/sub&gt; and ozone levels over the Eastern Atlantic and Western Europe using ship plume parameterization</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Huszar</surname>
<given-names>P.</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>Cariolle</surname>
<given-names>D.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Paoli</surname>
<given-names>R.</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>Halenka</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Belda</surname>
<given-names>M.</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>Schlager</surname>
<given-names>H.</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>Miksovsky</surname>
<given-names>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>Pisoft</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Department of Meteorology and Environment Protection, Faculty of Mathematics and Physics, Charles University, Prague, V Holešovičkách 2, Prague 8, 180 00, Czech Republic</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Centre Europeén de Recherche et de Formation Avancée en Calcul Scientifique, CERFACS/CNRS, Toulouse, France</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Météo-France, Toulouse, France</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Regular associate of the Abdus Salam ICTP, Trieste, Italy</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>German Aerospace Center, Institute of Atmospheric Physics, Oberpfaffenhofen-Wessling, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>21</day>
<month>07</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>14</issue>
<fpage>6645</fpage>
<lpage>6660</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>
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<abstract>
<p>In general, regional and global chemistry transport models apply
instantaneous mixing of emissions into the model&apos;s finest resolved scale. In
case of a concentrated source, this could result in erroneous calculation of
the evolution of both primary and secondary chemical species. Several studies
discussed this issue in connection with emissions from ships and aircraft.
In this study, we present an approach to deal with the non-linear effects
during dispersion of NO&lt;sub&gt;x&lt;/sub&gt; emissions from ships. It represents an adaptation
of the original approach developed for aircraft NO&lt;sub&gt;x&lt;/sub&gt; emissions, which uses
an exhaust tracer to trace the amount of the emitted species in the plume and
applies an effective reaction rate for the ozone production/destruction
during the plume&apos;s dilution into the background air. In accordance with
previous studies examining the impact of international shipping on the
composition of the troposphere, we found that the contribution of ship
induced surface NO&lt;sub&gt;x&lt;/sub&gt; to the total reaches 90% over remote ocean and makes
10–30% near coastal regions. Due to ship emissions, surface ozone increases
by up to 4–6 ppbv making 10% contribution to the surface ozone budget. When
applying the ship plume parameterization, we show that the large scale
NO&lt;sub&gt;x&lt;/sub&gt; decreases and the ship NO&lt;sub&gt;x&lt;/sub&gt; contribution is reduced by up to
20–25%. A similar decrease was found in the case of O&lt;sub&gt;3&lt;/sub&gt;. The plume
parameterization suppressed the ship induced ozone production by 15–30% over
large areas of the studied region. To evaluate the presented
parameterization, nitrogen monoxide measurements over the English Channel were
compared with modeled values and it was found that after activating the
parameterization the model accuracy increases.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
<body/>
<back>
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