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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>8</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-15375-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/15375/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/15375/2008/acpd-8-15375-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/15375/2008/acpd-8-15375-2008.pdf</fulltext_pdf>
	<start_page>15375</start_page>
	<end_page>15461</end_page>
	<publication_date>2008-08-14</publication_date>
	<article_title content_type="html">Evolution of Asian aerosols during transpacific transport in INTEX-B</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>E. J. Dunlea</name>
			<email>edward.dunlea@colorado.edu</email>
		</author>
		<author numeration="2" affiliations="1,2,12">
			<name>P. F. DeCarlo</name>
		</author>
		<author numeration="3" affiliations="1,3">
			<name>A. C. Aiken</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>J. R. Kimmel</name>
		</author>
		<author numeration="5" affiliations="4,13">
			<name>R. E. Peltier</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>R. J. Weber</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>J. Tomlison</name>
		</author>
		<author numeration="8" affiliations="5">
			<name>D. R. Collins</name>
		</author>
		<author numeration="9" affiliations="6">
			<name>Y. Shinozuka</name>
		</author>
		<author numeration="10" affiliations="6">
			<name>C. S. McNaughton</name>
		</author>
		<author numeration="11" affiliations="6">
			<name>S. G. Howell</name>
		</author>
		<author numeration="12" affiliations="6">
			<name>A. D. Clarke</name>
		</author>
		<author numeration="13" affiliations="7">
			<name>L. K. Emmons</name>
		</author>
		<author numeration="14" affiliations="7">
			<name>E. C. Apel</name>
		</author>
		<author numeration="15" affiliations="7">
			<name>G. G. Pfister</name>
		</author>
		<author numeration="16" affiliations="8">
			<name>A. van Donkelaar</name>
		</author>
		<author numeration="17" affiliations="8,9">
			<name>R. V. Martin</name>
		</author>
		<author numeration="18" affiliations="10">
			<name>D. B. Millet</name>
		</author>
		<author numeration="19" affiliations="11,14">
			<name>C. L. Heald</name>
		</author>
		<author numeration="20" affiliations="1,3">
			<name>J. L. Jimenez</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado, Boulder, CO 80309-0216, USA</affiliation>
		<affiliation numeration="2" content_type="html">Department of Atmospheric and Oceanic Science, University of Colorado, Boulder, CO 80309-0311, USA</affiliation>
		<affiliation numeration="3" content_type="html">Department of Chemistry and Biochemistry, University of Colorado, Boulder, CO 80309-0215, USA</affiliation>
		<affiliation numeration="4" content_type="html">School of Earth and Atmospheric Sciences, Georgia Inst. of Technology, Atlanta, GA, USA</affiliation>
		<affiliation numeration="5" content_type="html">Dept. of Atmospheric Sciences, Texas A&amp;M University, College Station, TX 77843, USA</affiliation>
		<affiliation numeration="6" content_type="html">Department of Oceanography, University of Hawaii, Honolulu, HI, USA</affiliation>
		<affiliation numeration="7" content_type="html">National Center for Atmospheric Research, P.O. Box 3000, Boulder, CO 80307-3000, USA</affiliation>
		<affiliation numeration="8" content_type="html">Department of Physics and Atmospheric Science, Dalhousie University Halifax, NS B3H 3J5, Canada</affiliation>
		<affiliation numeration="9" content_type="html">Harvard-Smithsonian Center for Astrophysics, Cambridge, MA, 02138, USA</affiliation>
		<affiliation numeration="10" content_type="html">Department of Soil, Water, and Climate, University of Minnesota, St. Paul, MN 55108, USA</affiliation>
		<affiliation numeration="11" content_type="html">Department of Chemistry, University of California – Berkeley, Berkeley, CA, 94720, USA</affiliation>
		<affiliation numeration="12" content_type="html">now at: Paul Scherrer Institute, CH-5232 Villigen-PSI, Switzerland</affiliation>
		<affiliation numeration="13" content_type="html">now at: NYU School of Medicine, Tuxedo, NY 10987, USA</affiliation>
		<affiliation numeration="14" content_type="html">now at: Department of Atmospheric Science, Colorado State University, Fort Collins, CO 80523, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Measurements of aerosol composition were made with an Aerodyne High
Resolution Time-of-Flight Aerosol Mass Spectrometer (HR-ToF-AMS) on board
the NSF/NCAR C-130 aircraft as part of the Intercontinental Chemical
Transport Experiment Phase B (INTEX-B) field campaign over the Eastern
Pacific Ocean. The HR-ToF-AMS measurements of non-refractory submicron
aerosol mass are shown to compare well with other aerosol instrumentation in
the INTEX-B field study. Two case studies are described for pollution layers
transported across the Pacific from the Asian continent, intercepted 3–4
days and 7–10 days downwind of Asia, respectively. Aerosol chemistry is
shown to be a robust tracer for air masses originating in Asia, specifically
the presence of sulfate dominated aerosol is a distinguishing feature of
Asian pollution layers that have been transported to the Eastern Pacific. We
examine the time scales of processing for sulfate and organic aerosol in the
atmosphere and show that our observations confirm a conceptual model for
transpacific transport from Asia proposed by Brock et al. (2004). Our
observations of both sulfate and organic aerosol in aged Asian pollution
layers are consistent with fast formation near the Asian continent, followed
by washout during lofting and subsequent transformation during transport
across the Pacific. Our observations are the first atmospheric measurements
to indicate that although secondary organic aerosol (SOA) formation from pollution happens on the timescale
of one day, the oxidation of organic aerosol continues at longer timescales
in the atmosphere. Comparisons with chemical transport models of data from
the entire campaign reveal an under-prediction of SOA mass in
the MOZART model, but much smaller discrepancies with the GEOS-Chem model
than found in previous studies over the Western Pacific. No evidence is
found to support a previous hypothesis for significant secondary organic
aerosol formation in the free troposphere.</abstract>
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</article>

