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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-9-9961-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/9961/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/9961/2009/acpd-9-9961-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/9961/2009/acpd-9-9961-2009.pdf</fulltext_pdf>
	<start_page>9961</start_page>
	<end_page>10013</end_page>
	<publication_date>2009-04-20</publication_date>
	<article_title content_type="html">Comparison of aerosol optical depths from the Ozone Monitoring Instrument (OMI) on Aura with results from airborne sunphotometry, other space and ground measurements during MILAGRO/INTEX-B</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. M. Livingston</name>
			<email>john.livingston@sri.com</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>J. Redemann</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>P. B. Russell</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>O. Torres</name>
		</author>
		<author numeration="5" affiliations="5">
			<name>B. Veihelmann</name>
		</author>
		<author numeration="6" affiliations="5">
			<name>P. Veefkind</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>R. Braak</name>
		</author>
		<author numeration="8" affiliations="6,7">
			<name>A. Smirnov</name>
		</author>
		<author numeration="9" affiliations="6">
			<name>L. Remer</name>
		</author>
		<author numeration="10" affiliations="2">
			<name>R. W. Bergstrom</name>
		</author>
		<author numeration="11" affiliations="8">
			<name>O. Coddington</name>
		</author>
		<author numeration="12" affiliations="8">
			<name>K. S. Schmidt</name>
		</author>
		<author numeration="13" affiliations="8">
			<name>P. Pilewskie</name>
		</author>
		<author numeration="14" affiliations="3">
			<name>R. Johnson</name>
		</author>
		<author numeration="15" affiliations="2">
			<name>Q. Zhang</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">SRI International, Menlo Park, CA, 94025, USA</affiliation>
		<affiliation numeration="2" content_type="html">Bay Area Environmental Research Institute (BAERI), Sonoma, CA, 95476, USA</affiliation>
		<affiliation numeration="3" content_type="html">NASA Ames Research Center, Moffett Field, CA, 94035, USA</affiliation>
		<affiliation numeration="4" content_type="html">Center for Atmospheric Sciences, Hampton University, Hampton, VA, 23668, USA</affiliation>
		<affiliation numeration="5" content_type="html">Royal Netherlands Meteorological Institute (KNMI), De Bilt, The Netherlands</affiliation>
		<affiliation numeration="6" content_type="html">NASA Goddard Space Flight Center, Greenbelt, MD, 20771, USA</affiliation>
		<affiliation numeration="7" content_type="html">Science Systems and Applications, Inc., Lanham, MD, 20706, USA</affiliation>
		<affiliation numeration="8" content_type="html">Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, CO, 80309, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Airborne sunphotometer measurements are used to evaluate retrievals of
extinction aerosol optical depth (AOD) from spatially coincident and
temporally near-coincident measurements by the Ozone Monitoring Instrument
(OMI) aboard the Aura satellite during the March 2006 Megacity
Initiative-Local And Global Research Observations/Phase B of the
Intercontinental Chemical Transport Experiment (MILAGRO/INTEX-B). The
14-channel NASA Ames Airborne Tracking Sunphotometer (AATS) flew on nine
missions over the Gulf of Mexico and four in or near the Mexico City area.
Retrievals of AOD from near-coincident AATS and OMI measurements are
compared for three flights over the Gulf of Mexico for flight segments when
the aircraft flew at altitudes 60–70 m a.s.l., and for one flight over Mexico
City when the aircraft flew ~420–590 m a.g.l. OMI-measured top of
atmosphere (TOA) reflectances are routinely inverted to yield aerosol
products such as AOD and aerosol absorption optical depth (AAOD) using two
different retrieval algorithms: a near-UV (OMAERUV) and a multiwavelength
(OMAERO) technique. This study uses the archived Collection 3 data products
from both algorithms. In particular, AATS and OMI AOD comparisons are
presented for AATS data acquired in 20 OMAERUV retrieval pixels (15 over
water) and 19 OMAERO pixels (also 15 over water). At least four pixels for
one of the over-water coincidences and all pixels for the over-land case
were cloud-free. Coincident AOD retrievals from 17 pixels of the Moderate
Resolution Imaging Spectroradiometer (MODIS) aboard Aqua are available for
two of the over-water flights and are shown to agree with AATS AODs to
within root mean square (RMS) differences of 0.00–0.06, depending on
wavelength. Near-coincident ground-based AOD measurements from ground-based
sun/sky radiometers operated as part of the Aerosol Robotic Network
(AERONET) at three sites in and near Mexico City are also shown and are
generally consistent with the AATS AODs (which exclude any AOD below the
aircraft) both in magnitude and spectral dependence. The OMAERUV algorithm
retrieves AODs corresponding to a non-absorbing aerosol model for all three
over-water comparisons, whereas the OMAERO algorithm retrieves best-fit AODs
corresponding to an absorbing biomass-burning aerosol model for two of the
three over-water cases. For the four cloud-free pixels in one over-water
coincidence (10 March), the OMAERUV retrievals underestimate the AATS AODs
by ~0.20, which exceeds the expected retrieval uncertainty, but
retrieved AODs agree with AATS values within uncertainties for the other two
over-water events. When OMAERO retrieves AODs corresponding to a
biomass-burning aerosol over water, the values significantly overestimate
the AATS AODs (by up to 0.55). For the Mexico City coincidence, comparisons
are presented for a non-urban region ~50–70 km northeast of the city
and for a site near the center of the city. OMAERUV retrievals are
consistent with AERONET AOD magnitudes for the non-urban site, but are
nearly double the AATS and AERONET AODs (with differences of up to 0.29) in
the center of the city. Corresponding OMAERO retrievals exceed the AATS
and/or AERONET AODs by factors of 3 to 10.</abstract>
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</article>

