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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>5</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-21785-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/21785/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/21785/2009/acpd-9-21785-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/21785/2009/acpd-9-21785-2009.pdf</fulltext_pdf>
	<start_page>21785</start_page>
	<end_page>21817</end_page>
	<publication_date>2009-10-16</publication_date>
	<article_title content_type="html">Absorption Angstrom Exponent in AERONET and related data as an indicator of aerosol composition</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>P. B. Russell</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>R. W. Bergstrom</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>Y. Shinozuka</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>A. D. Clarke</name>
		</author>
		<author numeration="5" affiliations="5,6,11">
			<name>P. F. DeCarlo</name>
		</author>
		<author numeration="6" affiliations="5,7">
			<name>J. L. Jimenez</name>
		</author>
		<author numeration="7" affiliations="8">
			<name>J. M. Livingston</name>
		</author>
		<author numeration="8" affiliations="2">
			<name>J. Redemann</name>
		</author>
		<author numeration="9" affiliations="9">
			<name>B. Holben</name>
		</author>
		<author numeration="10" affiliations="10">
			<name>O. Dubovik</name>
		</author>
		<author numeration="11" affiliations="1">
			<name>A. Strawa</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">NASA Ames Research Center, MS 245-5, Moffett Field, CA 94035-1000, USA</affiliation>
		<affiliation numeration="2" content_type="html">Bay Area Environmental Research Institute, 560 3rd Street West, Sonoma, CA 95476, USA</affiliation>
		<affiliation numeration="3" content_type="html">Oak Ridge Associated Universities, NASA Ames Research Center, MS 245-5, Moffett Field, CA  94035-1000, USA</affiliation>
		<affiliation numeration="4" content_type="html">School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu, HI, USA</affiliation>
		<affiliation numeration="5" content_type="html">Cooperative Institute for Research in the Environmental Sciences, University of Colorado, Boulder, Colorado, USA</affiliation>
		<affiliation numeration="6" content_type="html">Dept. of Atmospheric and Oceanic Sciences, University of Colorado, Boulder, Colorado, USA</affiliation>
		<affiliation numeration="7" content_type="html">Dept. of Chemistry and Biochemistry, University of Colorado, Boulder, Colorado, USA</affiliation>
		<affiliation numeration="8" content_type="html">SRI International, 333 Ravenswood Avenue, Menlo Park, CA 94025, USA</affiliation>
		<affiliation numeration="9" content_type="html">NASA Goddard Space Flight Center, Laboratory for Atmospheres, Code 912, Greenbelt, MD 20771, USA</affiliation>
		<affiliation numeration="10" content_type="html">Laboratoire d&apos;Optique Atmospherique, CNRS Universite de Lille, Bat 5, 59655 Villeneuve d&apos;Ascq CEDEX, France</affiliation>
		<affiliation numeration="11" content_type="html">now at: Laboratory of Atmospheric Chemistry, Paul Scherrer Institut, Villigen, Switzerland</affiliation>
	</affiliations>
	<abstract content_type="html">Recent results from diverse air, ground, and laboratory studies using both radiometric and
in situ techniques show that the fractions of black carbon, organic matter, and mineral dust
in atmospheric aerosols determine the wavelength dependence of absorption (expressed as
Absorption Angstrom Exponent, or AAE). Taken together, these results hold promise of
improving information on aerosol composition from remote measurements. The purpose of this
paper is to show that AAE values for Aerosol Robotic Network (AERONET) retrievals from
Sun-sky measurements describing the full aerosol vertical column are also strongly
correlated with aerosol composition or type. In particular, we find AAE values near 1 (the
theoretical value for black carbon) for AERONET-measured aerosol columns dominated by
urban-industrial aerosol, larger AAE values for biomass burning aerosols, and the largest
AAE values for Sahara dust aerosols. Ambiguities in aerosol composition or mixtures thereof,
resulting from intermediate AAE values, can be reduced via cluster analyses that supplement
AAE with other variables, for example Extinction Angstrom Exponent (EAE), which is an
indicator of particle size. Together with previous results, these results strengthen
prospects for determining aerosol composition from space, for example using the Glory
Aerosol Polarimetry Sensor (APS), which promises retrievals of multiwavelength
single-scattering albedo (SSA) and aerosol optical depth (and therefore aerosol absorption
optical depth (AAOD) and AAE), as well as shape and other aerosol properties. Cluster
analyses promise additional information content, for example by using the Ozone Monitoring
Instrument (OMI) to add AAOD in the near ultraviolet and CALIPSO aerosol layer heights to
reduce height-absorption ambiguity.</abstract>
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