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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>2</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-6571-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/6571/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/6571/2009/acpd-9-6571-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/6571/2009/acpd-9-6571-2009.pdf</fulltext_pdf>
	<start_page>6571</start_page>
	<end_page>6595</end_page>
	<publication_date>2009-03-10</publication_date>
	<article_title content_type="html">Particulate absorption of solar radiation: anthropogenic aerosols vs. dust</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>C. Wang</name>
			<email>wangc@mit.edu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>G.-R. Jeong</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>N. Mahowald</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Massachusetts Institute of Technology, Cambridge, MA 02139, USA</affiliation>
		<affiliation numeration="2" content_type="html">Cornell University, Ithaca, NY 14853, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Particulate solar absorption is a critical factor in determining the
      value and even sign of the direct radiative forcing of aerosols. The
      heating to the atmosphere and cooling to the Earth&apos;s surface caused by
      this absorption are hypothesized to have significant climate
      impacts. We find that anthropogenic aerosols play an important role
      around the globe in total particulate absorption of solar
      radiation. The global-average anthropogenic fraction in total aerosol
      absorbing optical depth exceeds 65% in all seasons. Combining the
      potentially highest dust absorption with the lowest anthropogenic
      absorption within our model range, this fraction would still exceed
      47% in most seasons except for boreal spring (36%) when dust
      abundance reaches its peak. Nevertheless, dust aerosol is still
      a critical absorbing constituent over places including North Africa,
      the entire tropical Atlantic, and during boreal spring in most part of
      Eurasian continent. The equality in absorbing solar radiation of dust
      and anthropogenic aerosols appears to be particularly important over
      Indian subcontinent and nearby regions as well as North Africa.</abstract>
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