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<article language="en">
	<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>9</volume_number>
		<issue_number>9</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acp-9-3223-2009</doi>
	<article_url>http://www.atmos-chem-phys.net/9/3223/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/9/3223/2009/acp-9-3223-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/9/3223/2009/acp-9-3223-2009.pdf</fulltext_pdf>
	<start_page>3223</start_page>
	<end_page>3231</end_page>
	<publication_date>2009-05-18</publication_date>
	<article_title content_type="html">Evidence of mineral dust altering cloud microphysics and precipitation</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>Q.-L. Min</name>
			<email>min@asrc.cestm.albany.edu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>R. Li</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>B. Lin</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>E. Joseph</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>S. Wang</name>
		</author>
		<author numeration="6" affiliations="2">
			<name>Y. Hu</name>
		</author>
		<author numeration="7" affiliations="3">
			<name>V. Morris</name>
		</author>
		<author numeration="8" affiliations="2">
			<name>F. Chang</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Atmospheric Sciences Research Center, State University of New York, USA</affiliation>
		<affiliation numeration="2" content_type="html">Science Directorate, NASA Langley Research Center, USA</affiliation>
		<affiliation numeration="3" content_type="html">NOAA Center for Atmospheric Sciences, Howard University, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Multi-platform and multi-sensor observations are employed to investigate the
impact of mineral dust on cloud microphysical and precipitation processes in
mesoscale convective systems. For a given convective strength, small
hydrometeors were more prevalent in the stratiform rain regions with dust
than in those regions that were dust free. Evidence of abundant cloud ice
particles in the dust sector, particularly at altitudes where heterogeneous
nucleation of mineral dust prevails, further supports the observed changes
of precipitation. The consequences of the microphysical effects of the dust
aerosols were to shift the precipitation size spectrum from heavy
precipitation to light precipitation and ultimately suppressing
precipitation.</abstract>
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</article>

