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	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>6</volume_number>
		<issue_number>9</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/acp-6-2593-2006</doi>
	<article_url>http://www.atmos-chem-phys.net/6/2593/2006/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/6/2593/2006/acp-6-2593-2006.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/6/2593/2006/acp-6-2593-2006.pdf</fulltext_pdf>
	<start_page>2593</start_page>
	<end_page>2649</end_page>
	<publication_date>2006-07-05</publication_date>
	<article_title content_type="html">The effect of physical and chemical aerosol properties on warm cloud droplet activation</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>G. McFiggans</name>
			<email>g.mcfiggans@manchester.ac.uk</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>P. Artaxo</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>U. Baltensperger</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>H. Coe</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>M. C. Facchini</name>
		</author>
		<author numeration="6" affiliations="5">
			<name>G. Feingold</name>
		</author>
		<author numeration="7" affiliations="4">
			<name>S. Fuzzi</name>
		</author>
		<author numeration="8" affiliations="1,3">
			<name>M. Gysel</name>
		</author>
		<author numeration="9" affiliations="6">
			<name>A. Laaksonen</name>
		</author>
		<author numeration="10" affiliations="7">
			<name>U. Lohmann</name>
		</author>
		<author numeration="11" affiliations="8">
			<name>T. F. Mentel</name>
		</author>
		<author numeration="12" affiliations="9">
			<name>D. M. Murphy</name>
		</author>
		<author numeration="13" affiliations="10">
			<name>C. D. O&apos;Dowd</name>
		</author>
		<author numeration="14" affiliations="11">
			<name>J. R. Snider</name>
		</author>
		<author numeration="15" affiliations="3">
			<name>E. Weingartner</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Atmospheric Sciences Group, SEAES, University of  Manchester, P.O. Box 88, Manchester, M60 1QD, UK</affiliation>
		<affiliation numeration="2" content_type="html">Instituto  de Fisica, Universidade de Sao Paulo, Rua do Matao, Travessa R, 187,  CEP 05508-900 Sao Paulo, Brazil</affiliation>
		<affiliation numeration="3" content_type="html">Paul Scherrer Institut,  Labor für Atmosphärenchemie, 5232 Villigen PSI,  Switzerland</affiliation>
		<affiliation numeration="4" content_type="html">Istituto di Scienze dell&apos;Atmosfera e del  Clima, CNR, 40129 Bologna, Italy</affiliation>
		<affiliation numeration="5" content_type="html">NOAA Environmental  Technology Laboratory, 325 Broadway, Boulder, Colorado 80305, USA</affiliation>
		<affiliation numeration="6" content_type="html">Department of Applied Physics, University of Kuopio, P.O. Box 1627, 70211 Kuopio, Finland</affiliation>
		<affiliation numeration="7" content_type="html">Institute for Atmospheric and  Climate Science, Schafmattstr. 30, ETH Zurich,  8093 Zurich, Switzerland</affiliation>
		<affiliation numeration="8" content_type="html">Forschungszentrum Jülich GmbH, ICG-II:  Troposphäre, 52425 Jülich,  Germany</affiliation>
		<affiliation numeration="9" content_type="html">NOAA Aeronomy Laboratory, 325 Broadway,  Boulder, Colorado  80305, USA</affiliation>
		<affiliation numeration="10" content_type="html">Department of Physics, National University  of Ireland, Galway, Ireland</affiliation>
		<affiliation numeration="11" content_type="html">University of Wyoming, Department of  Atmospheric Science, Laramie, WY 82071,  USA</affiliation>
	</affiliations>
	<abstract content_type="html">The effects of atmospheric aerosol on climate forcing may be very
substantial but are quantified poorly at present; in particular, the
effects of aerosols on cloud radiative properties, or the &quot;indirect
effects&quot; are credited with the greatest range of uncertainty amongst
the known causes of radiative forcing. This manuscript explores the
effects that the composition and properties of atmospheric aerosol
can have on the activation of droplets in warm clouds, so
potentially influencing the magnitude of the indirect effect. The
effects of size, composition, mixing state and various derived
properties are assessed and a range of these properties provided by
atmospheric measurements in a variety of locations is briefly
reviewed. The suitability of a range of process-level descriptions
to capture these aerosol effects is investigated by assessment of
their sensitivities to uncertainties in aerosol properties and by
their performance in closure studies. The treatment of these effects
within global models is reviewed and suggestions for future
investigations are made.</abstract>
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</article>

