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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-10-11681-2010</article-id>
<title-group>
<article-title>Present and future impact of aircraft, road traffic and shipping emissions on global tropospheric ozone</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Koffi</surname>
<given-names>B.</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>Szopa</surname>
<given-names>S.</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>Cozic</surname>
<given-names>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>Hauglustaine</surname>
<given-names>D.</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>van Velthoven</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Laboratoire des Sciences du Climat et de l&apos;Environnement, UMR 8212, IPSL, CEA-CNRS-UVSQ,  Gif-sur-Yvette, France</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Royal Netherlands Meteorological Institute, KNMI, De Bilt, The Netherlands</addr-line>
</aff>
<pub-date pub-type="epub">
<day>09</day>
<month>12</month>
<year>2010</year>
</pub-date>
<volume>10</volume>
<issue>23</issue>
<fpage>11681</fpage>
<lpage>11705</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/10/11681/2010/acp-10-11681-2010.html">This article is available from http://www.atmos-chem-phys.net/10/11681/2010/acp-10-11681-2010.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/10/11681/2010/acp-10-11681-2010.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/10/11681/2010/acp-10-11681-2010.pdf</self-uri>
<abstract>
<p>In this study, the LMDz-INCA climate-chemistry model and up-to-date global
emission inventories are used to investigate the &quot;present&quot; (2000) and future
(2050) impacts of transport emissions (road traffic, shipping and aircraft)
on global tropospheric ozone. For the first time, both impacts of emissions
and climate changes on transport-induced ozone are investigated. The 2000
transport emissions are shown to mainly affect ozone in the Northern Hemisphere, with
a maximum increase of the tropospheric column of up to 5 DU, from the South-eastern US to Central Europe. The impact is dominated by
road traffic in the middle and upper troposphere, North of 40Â° S, and by
shipping in the northern lower troposphere, over oceanic regions. A strong
reduction of road emissions and a moderate (B1 scenario) to high (A1B
scenario) increase of the ship and aircraft emissions are projected by the
year 2050. As a consequence, LMDz-INCA simulations predict a drastic
decrease in the impact of road emissions, whereas aviation would become the
major transport perturbation on tropospheric ozone, even in the case of a
very optimistic aircraft mitigation scenario. The A1B emission scenario
leads to an increase of the impact of transport on zonal mean ozone
concentrations in 2050 by up to +30% and +50%, in the Northern and
Southern Hemispheres, respectively. Despite a similar total amount of global
NO&lt;sub&gt;x&lt;/sub&gt; emissions by the various transport sectors compared to 2000, the
overall impact on the tropospheric ozone column is increased everywhere in
2050, due to a sectoral shift in the emissions of the respective transport
modes. On the opposite, the B1 mitigation scenario leads to a significant
reduction (by roughly 50%) of the ozone perturbation throughout the
troposphere compared to 2000.


&lt;br&gt;&lt;br&gt;

Considering climate change, and according to scenario A1B, a decrease of the
O&lt;sub&gt;3&lt;/sub&gt; tropospheric burden is simulated by 2050 due to climate change (âˆ’1.2%), whereas an increase of ozone of up to 2% is calculated in the
upper troposphere in the inter-tropical zone, due to enhanced lightning
activity. A global impact of similar magnitude is simulated for the
transport-induced ozone burden perturbation (âˆ’1.6%). As a result, the
future increase in global ozone due to changes in anthropogenic emissions is
lowered by 12% and by 4%, for the background and the transport-induced
ozone, respectively. However, positive and negative climate effects are
obtained on ozone, depending on the season, region and altitude, with an
increase of the transport-induced ozone perturbation (+0.4 DU) in the
already most affected area of Northern Hemisphere.</p>
</abstract>
<counts><page-count count="25"/></counts>
</article-meta>
</front>
<body/>
<back>
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