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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-9-9417-2009</article-id>
<title-group>
<article-title>The influence of the vertical distribution of emissions on tropospheric chemistry</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pozzer</surname>
<given-names>A.</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>JÃ¶ckel</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</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>Van Aardenne</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>The Cyprus Institute, Energy, Environment and Water Research Centre, Nicosia, Cyprus</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Max-Planck Institute of Chemistry, Air Chemistry Department, Mainz, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>European Commission, DG Joint Research Centre, Ispra, Italy</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>now at: Deutsches Zentrum fuer Luft- und Raumfahrt, Oberpfaffenhofen, Wessling, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>15</day>
<month>12</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>24</issue>
<fpage>9417</fpage>
<lpage>9432</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/9/9417/2009/acp-9-9417-2009.html">This article is available from http://www.atmos-chem-phys.net/9/9417/2009/acp-9-9417-2009.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/9/9417/2009/acp-9-9417-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/9/9417/2009/acp-9-9417-2009.pdf</self-uri>
<abstract>
<p>The atmospheric chemistry general circulation model EMAC (ECHAM5/MESSy
atmospheric chemistry) is used to investigate
the effect of height dependent emissions
on tropospheric chemistry.
In a sensitivity simulation,
anthropogenic and biomass burning emissions
are released in the lowest model layer.
The resulting tracer distributions are compared to those of a former
simulation applying height dependent emissions.
Although the differences between the two simulations
in the free troposphere are small
(less than 5%), large differences are present in polluted regions
at the surface, in particular for NO&lt;sub&gt;x&lt;/sub&gt; (more than 100%),
CO (up to 30%)  and
non-methane hydrocarbons (up to 30%), whereas for OH the differences at the
same locations are somewhat lower (15%).
Global ozone formation is virtually unaffected by the choice of the vertical
distribution of emissions.
Nevertheless, local ozone changes can be up to 30%.
Model results of both simulations are further compared to observations
from field campaigns and to data from measurement stations.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
<body/>
<back>
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