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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-12-961-2012</article-id>
<title-group>
<article-title>Distributions and regional budgets of aerosols and their precursors simulated with the EMAC chemistry-climate model</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>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>de Meij</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>Pringle</surname>
<given-names>K. J.</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>Tost</surname>
<given-names>H.</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>Doering</surname>
<given-names>U. M.</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>van Aardenne</surname>
<given-names>J.</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>Lelieveld</surname>
<given-names>J.</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="aff7">
<sup>7</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>The Cyprus Institute, Energy, Environment and Water Research Center, P.O. Box 27456, 1645 Nicosia, Cyprus</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Atmospheric Chemistry Department, Max-Planck Institute of Chemistry, P.O. Box 3060, 55020 Mainz, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>School of Earth and Environment, Univ. of Leeds, Woodhouse Lane, Leeds, LS2 9JT, UK</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Institut für Physik der Atmosphere, Johannes-Gutenberg Universität Mainz, 55099, Mainz, Germany</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Federal Environment Agency (UBA), Wörlitzer Platz 1, 06844, Dessau, Germany</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>European Commission Joint Research Centre, Institute for Environment and Sustainability, Ispra, Italy</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>King Saud University, Riyadh 11451, Saudi Arabia</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>now at: The Abdus Salam International center for Theoretical Physics,   Earth System Physics section, Strada Costiera 11, 34151 Trieste, Italy</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>now at: Air and climate change-mitigation, European Environment Agency, Kongens Nytorv 6, 1050 Copenhagen K, Denmark</addr-line>
</aff>
<pub-date pub-type="epub">
<day>19</day>
<month>01</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>2</issue>
<fpage>961</fpage>
<lpage>987</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/12/961/2012/acp-12-961-2012.html">This article is available from http://www.atmos-chem-phys.net/12/961/2012/acp-12-961-2012.html</self-uri>
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<abstract>
<p>The new global anthropogenic emission inventory
      (EDGAR-CIRCE) of gas and aerosol pollutants has been incorporated in
      the chemistry general circulation model EMAC (ECHAM5/MESSy Atmospheric
      Chemistry).  A relatively high horizontal resolution simulation is performed for
      the years 2005–2008 to evaluate the capability of the model and the
      emissions to reproduce observed aerosol concentrations and aerosol
      optical depth (AOD) values.  Model output is compared with
      observations from different measurement networks (CASTNET, EMEP and
      EANET) and AODs from remote sensing instruments (MODIS and MISR).
      A good spatial agreement of the distribution of sulfate and ammonium aerosol
      is found when compared to observations, while calculated nitrate
      aerosol concentrations show some discrepancies.  The simulated
      temporal development of the inorganic aerosols is in line with
      measurements of sulfate and nitrate aerosol, while for ammonium
      aerosol some deviations from observations occur over the USA,
      due to the wrong temporal distribution of ammonia gas emissions.
      The calculated AODs agree well with the satellite observations in most
      regions, while negative biases are found for the equatorial area and in
      the dust outflow regions (i.e. Central Atlantic and Northern Indian
      Ocean), due to an underestimation of biomass burning and aeolian dust
      emissions, respectively.
      Aerosols and precursors budgets for five different regions
      (North America, Europe, East Asia, Central Africa and South America)
      are calculated. Over East-Asia most of the emitted aerosols (precursors) are also
      deposited within the region, while in North America and Europe
      transport plays a larger role.
      Further, it is shown that a simulation with monthly varying anthropogenic
      emissions typically improves the temporal correlation
      by 5–10% compared to one with constant annual emissions.</p>
</abstract>
<counts><page-count count="27"/></counts>
</article-meta>
</front>
<body/>
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