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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>2</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-8143-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/8143/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/8143/2008/acpd-8-8143-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/8143/2008/acpd-8-8143-2008.pdf</fulltext_pdf>
	<start_page>8143</start_page>
	<end_page>8191</end_page>
	<publication_date>2008-04-24</publication_date>
	<article_title content_type="html">Transpacific transport of ozone pollution and the effect of recent Asian emission increases on air quality in North America: an integrated analysis using satellite, aircraft, ozonesonde, and surface observations</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>L. Zhang</name>
			<email>linzhang@fas.harvard.edu</email>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>D. J. Jacob</name>
		</author>
		<author numeration="3" affiliations="2,15">
			<name>K. F. Boersma</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>D. A. Jaffe</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>J. R. Olson</name>
		</author>
		<author numeration="6" affiliations="5">
			<name>K. W. Bowman</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>J. R. Worden</name>
		</author>
		<author numeration="8" affiliations="6">
			<name>A. M. Thompson</name>
		</author>
		<author numeration="9" affiliations="4">
			<name>M. A. Avery</name>
		</author>
		<author numeration="10" affiliations="7">
			<name>R. C. Cohen</name>
		</author>
		<author numeration="11" affiliations="8">
			<name>J. E. Dibb</name>
		</author>
		<author numeration="12" affiliations="9">
			<name>F. M. Flocke</name>
		</author>
		<author numeration="13" affiliations="10">
			<name>H. E. Fuelberg</name>
		</author>
		<author numeration="14" affiliations="11">
			<name>L. G. Huey</name>
		</author>
		<author numeration="15" affiliations="12">
			<name>W. W. McMillan</name>
		</author>
		<author numeration="16" affiliations="13">
			<name>H. B. Singh</name>
		</author>
		<author numeration="17" affiliations="14">
			<name>A. J. Weinheimer</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Dept. of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, USA</affiliation>
		<affiliation numeration="2" content_type="html">School of Engineering and Applied Sciences, Harvard Univ., Cambridge, MA 02138, USA</affiliation>
		<affiliation numeration="3" content_type="html">University of Washington, 18115 Campus Way NE, Bothell, WA 98021, USA</affiliation>
		<affiliation numeration="4" content_type="html">Atmospheric Sciences Division, Langley Research Center, NASA, Hampton, VA 23681, USA</affiliation>
		<affiliation numeration="5" content_type="html">Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, CA 91109, USA</affiliation>
		<affiliation numeration="6" content_type="html">The Pennsylvania State University, Department of Meteorology, 503 Walker Building, University Park, PA 16802-5013 USA</affiliation>
		<affiliation numeration="7" content_type="html">Department of Chemistry, University of California, Berkeley, CA 94720, USA</affiliation>
		<affiliation numeration="8" content_type="html">University of New Hampshire, Climate Change Research Center, 39 College Road, Durham, NH 03824, USA</affiliation>
		<affiliation numeration="9" content_type="html">Earth Observing Lab., National Center for Atmospheric Research, Boulder, CO 80307, USA</affiliation>
		<affiliation numeration="10" content_type="html">Department of Meteorology, Florida State University, Tallahassee, FL 32306-4520, USA</affiliation>
		<affiliation numeration="11" content_type="html">School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332-0340, USA</affiliation>
		<affiliation numeration="12" content_type="html">Department of Physics, University of Maryland Baltimore County, 1000 Hilltop Circle, Baltimore, MD 21250, USA</affiliation>
		<affiliation numeration="13" content_type="html">NASA Ames Research Center, MS-245-5, Moffett Field, CA 94035, USA</affiliation>
		<affiliation numeration="14" content_type="html">National Center for Atmospheric Res., 1850 Table Mesa Drive, Boulder, CO 80305, USA</affiliation>
		<affiliation numeration="15" content_type="html">now at: KNMI, PO Box 201, 3730 AE De Bilt, The Netherlands</affiliation>
	</affiliations>
	<abstract content_type="html">We use an ensemble of aircraft, satellite, sonde, and surface observations
for April&amp;ndash;May 2006 (NASA/INTEX-B aircraft campaign) to better understand the
mechanisms for transpacific ozone pollution and its implications for North
American air quality. The observations are interpreted with a global 3-D
chemical transport model (GEOS-Chem). OMI NO&lt;sub&gt;2&lt;/sub&gt; satellite observations
constrain Asian anthropogenic NO&lt;sub&gt;x&lt;/sub&gt; emissions and indicate a factor of 2
increase from 2000 to 2006 in China. Satellite observations of CO from AIRS
and TES indicate two major events of Asian transpacific pollution during
INTEX-B. Correlation between TES CO and ozone observations shows evidence
for transpacific ozone pollution. The semi-permanent Pacific High and
Aleutian Low cause splitting of transpacific pollution plumes over the
Northeast Pacific. The northern branch circulates around the Aleutian Low
and has little impact on North America. The southern branch circulates
around the Pacific High and impacts western North America. Both aircraft
measurements and model results show sustained ozone production driven by
peroxyacetylnitrate (PAN) decomposition in the southern branch, roughly
doubling the transpacific influence from ozone produced in the Asian
boundary layer. Model simulation of ozone observations at Mt. Bachelor
Observatory in Oregon (2.7 km altitude) indicates a mean Asian ozone
pollution contribution of 9&amp;plusmn;3 ppbv to the mean observed concentration
of 54 ppbv, reflecting mostly an enhancement in background ozone rather than
episodic Asian plumes. Asian pollution enhanced surface ozone concentrations
by 5&amp;ndash;7 ppbv over western North America in spring 2006. The 2000&amp;ndash;2006 rise in
Asian anthropogenic emissions increased the influence by 1&amp;ndash;2 ppbv.</abstract>
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