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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>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-13-3569-2013</article-id>
<title-group>
<article-title>The relative importance of impacts from climate change vs. emissions change on air pollution levels in the 21st century</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hedegaard</surname>
<given-names>G. B.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<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>Christensen</surname>
<given-names>J. H.</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>Brandt</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Aarhus University, Department of Environmental Science, Roskilde,  Denmark</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Danish Climate Center, Danish Meteorological Institute,  Copenhagen, Denmark</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>now at: Center for Climate and Environmental  Research, Lund University, Lund, Sweden</addr-line>
</aff>
<pub-date pub-type="epub">
<day>02</day>
<month>04</month>
<year>2013</year>
</pub-date>
<volume>13</volume>
<issue>7</issue>
<fpage>3569</fpage>
<lpage>3585</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 G. B. Hedegaard et al.</copyright-statement>
<copyright-year>2013</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://acp.copernicus.org/articles/13/3569/2013/acp-13-3569-2013.html">This article is available from https://acp.copernicus.org/articles/13/3569/2013/acp-13-3569-2013.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/13/3569/2013/acp-13-3569-2013.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/13/3569/2013/acp-13-3569-2013.pdf</self-uri>
<abstract>
<p>So far several studies have analysed the impacts of climate change on future
air pollution levels. Significant changes due to impacts of climate change
have been made clear. Nevertheless, these changes are not yet included in
national, regional or global air pollution reduction strategies. The changes
in future air pollution levels are caused by both impacts from climate change
and anthropogenic emission changes, the importance of which needs
to be quantified and compared. In this study we use the Danish Eulerian
Hemispheric Model (DEHM) driven by meteorological input data from the coupled
Atmosphere-Ocean General Circulation Model ECHAM5/MPI-OM and forced with the
newly developed RCP4.5 emissions. The relative importance of the climate
signal and the signal from changes in anthropogenic emissions on the future
ozone, black carbon (BC), total particulate matter with a diameter below
2.5 μm (total PM&lt;sub&gt;2.5&lt;/sub&gt; including BC, primary organic carbon
(OC), mineral dust and secondary inorganic aerosols (SIA)) and total nitrogen
(including NH&lt;sub&gt;x&lt;/sub&gt; + NO&lt;sub&gt;y&lt;/sub&gt;) has been determined. For ozone, the
impacts of anthropogenic emissions dominate, though a climate penalty is
found in the Arctic region and northwestern Europe, where the signal from
climate change dampens the effect from the projected emission reductions of
anthropogenic ozone precursors. The investigated particles are even more
dominated by the impacts from emission changes. For black carbon the emission
signal dominates slightly at high latitudes, with an increase up to an order
of magnitude larger, close to the emission sources in temperate and
subtropical areas. Including all particulate matter with a diameter below
2.5 μm (total PM&lt;sub&gt;2.5&lt;/sub&gt;) enhances the dominance from emissions
change. In contrast, total nitrogen (NH&lt;sub&gt;x&lt;/sub&gt; + NO&lt;sub&gt;y&lt;/sub&gt;) in parts
of the Arctic and at low latitudes is dominated by impacts of climate change.</p>
</abstract>
<counts><page-count count="17"/></counts>
</article-meta>
</front>
<body/>
<back>
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