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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>10</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/acpd-10-763-2010</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/10/763/2010/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/10/763/2010/acpd-10-763-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/10/763/2010/acpd-10-763-2010.pdf</fulltext_pdf>
	<start_page>763</start_page>
	<end_page>783</end_page>
	<publication_date>2010-01-15</publication_date>
	<article_title content_type="html">Longwave indirect effect of mineral dusts on ice clouds</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>Q. Min</name>
			<email>min@asrc.cestm.albany.edu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>R. Li</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Atmospheric Sciences Research Center, State University of New York,  Albany, NY 12203, USA</affiliation>
	</affiliations>
	<abstract content_type="html">In addition to microphysical changes in clouds, changes in
      nucleation processes of ice cloud due to aerosols would result
      in substantial changes in cloud top distribution as mildly
      supercooled clouds are glaciated through heterogonous
      nucleation processes. Measurements from multiple sensors on
      multiple observing platforms over the Atlantic Ocean show that
      the cloud effective temperature increases with mineral dust
      loading with a slope of +3.06 &amp;deg;C per unit AOD. The
      macrophysical changes in ice cloud top distributions as
a consequence of mineral dust-cloud interaction exert a strong
      cooling effect (up to 16 w m&lt;sup&gt;&amp;minus;2&lt;/sup&gt;) of thermal infrared
      radiation on cloud systems. Induced changes of ice particle
      size by mineral dusts influence cloud emissivity and play
      a minor role in modulating the outgoing longwave radiation for
      optically thin ice clouds. Such a strong cooling forcing of
      thermal infrared radiation would have significant impacts on
      cloud systems and subsequently on climate.</abstract>
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