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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>8</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-12721-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/12721/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/12721/2008/acpd-8-12721-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/12721/2008/acpd-8-12721-2008.pdf</fulltext_pdf>
	<start_page>12721</start_page>
	<end_page>12736</end_page>
	<publication_date>2008-07-04</publication_date>
	<article_title content_type="html">Cloud processing, cloud evaporation and Angström exponent</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>G.-J. Roelofs</name>
			<email>g.j.h.roelofs@uu.nl</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>V. Kamphuis</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute for Marine and Atmospheric Research Utrecht (IMAU), Utrecht University, Princetonplein 5, 3584 CC Utrecht, The Netherlands</affiliation>
	</affiliations>
	<abstract content_type="html">With a cloud parcel model we investigated how cloud processing and cloud
evaporation modify the size distribution and the Angström exponent of an
aerosol population. Cloud processing causes a decrease in particle
concentrations, relatively most efficiently in the coarse mode, and reduces
the relative dispersion of the aerosol distribution. As a result the
Angström exponent of the aerosol increases. The Angström exponent is
subject to other influences. It is very sensitive for relative humidity,
especially between 95% and 100%. In addition, kinetic limitations
delay droplet evaporation during cloud dissipation, which hampers a direct
relation between the Angström exponent and the relative humidity.
Consequently, a direct interpretation of the Angström exponent in terms
of aerosol properties that play a role in aerosol-cloud interactions, such
as the fine mode fraction, is rather complex.</abstract>
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