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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-7-3425-2007</article-id>
<title-group>
<article-title>Cloud microphysics and aerosol indirect effects in the global climate model ECHAM5-HAM</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lohmann</surname>
<given-names>U.</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>Stier</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hoose</surname>
<given-names>C.</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>Ferrachat</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>Kloster</surname>
<given-names>S.</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>Roeckner</surname>
<given-names>E.</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>Zhang</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Atmospheric and Climate Science,  ETH Zurich, Switzerland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Environmental Science and Engineering, California Institute of Technology, Pasadena, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>EC, Joint Research Centre, IES, Climate Change Unit, Ispra, Italy</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Max Planck Institute for Meteorology, Hamburg, Germany</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Meteorological Service of Canada, Toronto, Canada</addr-line>
</aff>
<pub-date pub-type="epub">
<day>02</day>
<month>07</month>
<year>2007</year>
</pub-date>
<volume>7</volume>
<issue>13</issue>
<fpage>3425</fpage>
<lpage>3446</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/7/3425/2007/acp-7-3425-2007.html">This article is available from http://www.atmos-chem-phys.net/7/3425/2007/acp-7-3425-2007.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/7/3425/2007/acp-7-3425-2007.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/7/3425/2007/acp-7-3425-2007.pdf</self-uri>
<abstract>
<p>The double-moment cloud microphysics scheme from ECHAM4 that
  predicts both the mass mixing ratios and number concentrations of
  cloud droplets and ice crystals  has been coupled to the size-resolved aerosol scheme
ECHAM5-HAM.  ECHAM5-HAM predicts the  aerosol mass, number
concentrations and mixing state. The simulated  liquid, ice and total water content
and the cloud droplet and ice crystal number concentrations as a
function of temperature in stratiform mixed-phase clouds between 0 and
&amp;minus;35&amp;deg; C agree much better with aircraft observations in the ECHAM5
simulations. ECHAM5 performs better because more realistic aerosol
concentrations are available for cloud droplet nucleation and because
the Bergeron-Findeisen process is parameterized as being more
efficient.

&lt;br&gt;&lt;br&gt;
The total anthropogenic aerosol effect includes the direct,
semi-direct and indirect effects and is defined as the difference in
the top-of-the-atmosphere net radiation between present-day and
pre-industrial times. It amounts to &amp;minus;1.9 W m&lt;sup&gt;&amp;minus;2&lt;/sup&gt; in ECHAM5, when a
relative humidity dependent cloud cover scheme and aerosol
emissions representative for the years 1750 and 2000 from the AeroCom
emission inventory are used. The contribution
of the cloud albedo effect amounts to &amp;minus;0.7 W m&lt;sup&gt;&amp;minus;2&lt;/sup&gt;.
The total anthropogenic aerosol effect is larger when
either a statistical cloud cover scheme or a different aerosol
emission inventory are employed because the cloud lifetime
effect increases.</p>
</abstract>
<counts><page-count count="22"/></counts>
</article-meta>
</front>
<body/>
<back>
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