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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</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/acpd-9-24717-2009</article-id>
<title-group>
<article-title>Comprehensively accounting for the effect of giant CCN in cloud droplet activation parameterizations</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Barahona</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>West</surname>
<given-names>R. E. L.</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>Stier</surname>
<given-names>P.</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>Romakkaniemi</surname>
<given-names>S.</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>Kokkola</surname>
<given-names>H.</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>Nenes</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-group><aff id="aff1">
<label>1</label>
<addr-line>School of Chemical and Biomolecular Engineering, Georgia Institute of Technology, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>School of Earth and Atmospheric Sciences, Georgia Institute of Technology, USA</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Atmospheric, Oceanic and Planetary Physics, Department of Physics, University\newline of Oxford, UK</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Department of Physics, University of Kuopio, Finland</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Finnish Meteorological Institute, Kuopio Unit, Finland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>18</day>
<month>11</month>
<year>2009</year>
</pub-date>
<volume>9</volume>
<issue>6</issue>
<fpage>24717</fpage>
<lpage>24730</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-discuss.net/9/24717/2009/acpd-9-24717-2009.html">This article is available from http://www.atmos-chem-phys-discuss.net/9/24717/2009/acpd-9-24717-2009.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/9/24717/2009/acpd-9-24717-2009.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/9/24717/2009/acpd-9-24717-2009.pdf</self-uri>
<abstract>
<p>Cloud droplet activation parameterizations used in aerosol
      indirect effect assessments often assume that droplet growth
      after activation is much greater than their equilibrium size
      close to cloud base. This assumption does not hold for large
      CCN which may experience limited growth. If a large fraction of the aerosol is composed of
      such particles (such as regions with large fractions of dust
      particles and seasalt), neglecting such kinetic limitations in
      cloud droplet activation parameterizations leads to an
      underestimation of droplet surface area during cloud
      formation, hence overestimation of maximum supersaturation and
      cloud droplet number. Here we present a simple approach to
      address this problem and that can easily be incorporated into
      cloud droplet activation parameterizations. A demonstration of
      this method is done for activation parameterizations based on
      the &apos;&apos;population splitting&apos;&apos; concept of Nenes and Seinfeld
      (2003).</p>
</abstract>
<counts><page-count count="14"/></counts>
</article-meta>
</front>
<body/>
<back>
<ref-list>
<title>References</title>
<ref id="ref1">
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<label>2</label><mixed-citation publication-type="other" xlink:type="simple"> Barahona,~D. and Nenes,~A.: Parameterization of cloud droplet formation in large scale models: including effects of entrainment, J. Geophys. Res., J. Geophys. Res., 112, D16206, doi:10.1029/2007JD008473, 2007. </mixed-citation>
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<label>6</label><mixed-citation publication-type="other" xlink:type="simple"> Feingold,~G. and Heymsfield,~A J.: Parameterization of condensational growth of droplets for use in general circulation models, J. Atmos. Sci., 49, 2325–2342, 1992. </mixed-citation>
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<label>7</label><mixed-citation publication-type="other" xlink:type="simple"> Fountoukis,~C. and Nenes,~A.: Continued development of a~cloud droplet formation parameterization for global climate models, J. Geophys. Res., 110, D11212, \doi11210.11029/12004JD005591, 2005. </mixed-citation>
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<ref id="ref8">
<label>8</label><mixed-citation publication-type="other" xlink:type="simple"> Kumar, P., Sokolik, I. N., and Nenes, A.: Parameterization of cloud droplet formation for global and regional models: including adsorption activation from insoluble CCN, Atmos. Chem. Phys., 9, 2517–2532, 2009.  </mixed-citation>
</ref>
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</ref>
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<label>12</label><mixed-citation publication-type="other" xlink:type="simple"> Nenes,~A. and Seinfeld,~J H.: Parameterization of cloud droplet formation in global climate models, J. Geophys. Res., 108, 4415, \doi4410.1029/2002JD002911, 2003. </mixed-citation>
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</ref-list>
</back>
</article>