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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>9</volume_number>
		<issue_number>6</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-24717-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/24717/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/24717/2009/acpd-9-24717-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/24717/2009/acpd-9-24717-2009.pdf</fulltext_pdf>
	<start_page>24717</start_page>
	<end_page>24730</end_page>
	<publication_date>2009-11-18</publication_date>
	<article_title content_type="html">Comprehensively accounting for the effect of giant CCN in cloud droplet activation parameterizations</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>D. Barahona</name>
		</author>
		<author numeration="2" affiliations="3">
			<name>R. E. L. West</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>P. Stier</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>S. Romakkaniemi</name>
		</author>
		<author numeration="5" affiliations="5">
			<name>H. Kokkola</name>
		</author>
		<author numeration="6" affiliations="1,2">
			<name>A. Nenes</name>
			<email>athanasios.nenes@gatech.edu</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">School of Chemical and Biomolecular Engineering, Georgia Institute of Technology, USA</affiliation>
		<affiliation numeration="2" content_type="html">School of Earth and Atmospheric Sciences, Georgia Institute of Technology, USA</affiliation>
		<affiliation numeration="3" content_type="html">Atmospheric, Oceanic and Planetary Physics, Department of Physics, University\newline of Oxford, UK</affiliation>
		<affiliation numeration="4" content_type="html">Department of Physics, University of Kuopio, Finland</affiliation>
		<affiliation numeration="5" content_type="html">Finnish Meteorological Institute, Kuopio Unit, Finland</affiliation>
	</affiliations>
	<abstract content_type="html">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).</abstract>
	<references>
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	</references>
</article>

