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<article language="en">
	<journal>
		<journal_title>Atmospheric Measurement Techniques Discussions</journal_title>
		<journal_url>www.atmos-meas-tech-discuss.net</journal_url>
		<eissn>1867-8610</eissn>
		<volume_number>3</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/amtd-3-3319-2010</doi>
	<article_url>http://www.atmos-meas-tech-discuss.net/3/3319/2010/</article_url>
	<abstract_html>http://www.atmos-meas-tech-discuss.net/3/3319/2010/amtd-3-3319-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-meas-tech-discuss.net/3/3319/2010/amtd-3-3319-2010.pdf</fulltext_pdf>
	<start_page>3319</start_page>
	<end_page>3344</end_page>
	<publication_date>2010-08-09</publication_date>
	<article_title content_type="html">Intercomparison of CALIOP and MODIS aerosol optical depth retrievals</article_title>
	<authors>
		<author numeration="1" affiliations="1,4">
			<name>C. Kittaka</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>D. M. Winker</name>
			<email>david.m.winker@nasa.gov</email>
		</author>
		<author numeration="3" affiliations="2">
			<name>M. A. Vaughan</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>A. Omar</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>L. A. Remer</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Science Systems and Applications Inc., Hampton, VA, USA</affiliation>
		<affiliation numeration="2" content_type="html">NASA Langley Research Center, Hampton, VA, USA</affiliation>
		<affiliation numeration="3" content_type="html">NASA Goddard Spaceflight Center, Greenbelt, MD, USA</affiliation>
		<affiliation numeration="4" content_type="html">deceased</affiliation>
	</affiliations>
	<abstract content_type="html">The Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) is carried on
the CALIPSO satellite and has acquired global aerosol profiles since June 2006.
CALIPSO is flown in formation with the Aqua satellite as part of the
A-train satellite constellation, so that a large number of coincident
aerosol observations are available from CALIOP and the MODIS-Aqua
instrument. This study compares column aerosol optical depth at 0.532 μm
derived from CALIOP aerosol profiles with MODIS-Aqua 0.55 μm aerosol
optical depth over the period June 2006 through August 2008. The study is
based on the CALIOP Version 2 Aerosol Layer Product and MODIS Collection 5.
While CALIOP is first and foremost a profiling instrument, this comparison
of column aerosol optical depth provides insight into quality of CALIOP
aerosol data. It is found that daytime aerosol optical depth from the CALIOP
Version 2 product has a small global mean bias relative to MODIS Collection
5. Regional biases, of both signs, are larger and biases are seen to vary
somewhat with season. In northern mid-latitudes, aerosol optical depth from
CALIOP is lower, on average, than from MODIS. This may be partly due to a
latitude-dependent calibration error in Version 2 CALIOP Level 1 daytime
0.532 μm profiles. This comparison of CALIOP and MODIS also provides
insight into possible biases in the MODIS aerosol optical depth product due
to cloud masking and errors in modeling land surface reflectance.</abstract>
	<references>
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</article>

