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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>10</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/acp-10-977-2010</doi>
	<article_url>http://www.atmos-chem-phys.net/10/977/2010/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/10/977/2010/acp-10-977-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/10/977/2010/acp-10-977-2010.pdf</fulltext_pdf>
	<start_page>977</start_page>
	<end_page>996</end_page>
	<publication_date>2010-02-01</publication_date>
	<article_title content_type="html">Source attribution and interannual variability of Arctic pollution in spring constrained by aircraft (ARCTAS, ARCPAC) and satellite (AIRS) observations of carbon monoxide</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. A. Fisher</name>
			<email>jafisher@fas.harvard.edu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>D. J. Jacob</name>
		</author>
		<author numeration="3" affiliations="1,14">
			<name>M. T. Purdy</name>
		</author>
		<author numeration="4" affiliations="1,15">
			<name>M. Kopacz</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>P. Le Sager</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>C. Carouge</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>C. D. Holmes</name>
		</author>
		<author numeration="8" affiliations="1">
			<name>R. M. Yantosca</name>
		</author>
		<author numeration="9" affiliations="2">
			<name>R. L. Batchelor</name>
		</author>
		<author numeration="10" affiliations="2">
			<name>K. Strong</name>
		</author>
		<author numeration="11" affiliations="3">
			<name>G. S. Diskin</name>
		</author>
		<author numeration="12" affiliations="4">
			<name>H. E. Fuelberg</name>
		</author>
		<author numeration="13" affiliations="5,6">
			<name>J. S. Holloway</name>
		</author>
		<author numeration="14" affiliations="7">
			<name>E. J. Hyer</name>
		</author>
		<author numeration="15" affiliations="8,9">
			<name>W. W. McMillan</name>
		</author>
		<author numeration="16" affiliations="9">
			<name>J. Warner</name>
		</author>
		<author numeration="17" affiliations="10">
			<name>D. G. Streets</name>
		</author>
		<author numeration="18" affiliations="10,11">
			<name>Q. Zhang</name>
		</author>
		<author numeration="19" affiliations="12">
			<name>Y. Wang</name>
		</author>
		<author numeration="20" affiliations="13">
			<name>S. Wu</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Earth and Planetary Sciences and School of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts, USA</affiliation>
		<affiliation numeration="2" content_type="html">Department of Physics, University of Toronto, Toronto, Ontario, Canada</affiliation>
		<affiliation numeration="3" content_type="html">NASA Langley Research Center, Hampton, Virginia, USA</affiliation>
		<affiliation numeration="4" content_type="html">Department of Meteorology, Florida State University, Tallahassee, Florida, USA</affiliation>
		<affiliation numeration="5" content_type="html">Cooperative Institute for Research in Environmental Science, University of Colorado, Boulder, Colorado, USA</affiliation>
		<affiliation numeration="6" content_type="html">Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, Colorado, USA</affiliation>
		<affiliation numeration="7" content_type="html">UCAR Visiting Scientist Program, Naval Research Laboratory, Monterey, California, USA</affiliation>
		<affiliation numeration="8" content_type="html">Department of Physics, University of Maryland, Baltimore County, Baltimore, Maryland, USA</affiliation>
		<affiliation numeration="9" content_type="html">Joint Center for Earth Systems Technology, University of Maryland, Baltimore, Maryland, USA</affiliation>
		<affiliation numeration="10" content_type="html">Decision and Information Sciences Division, Argonne National Laboratory, Argonne, Illinois, USA</affiliation>
		<affiliation numeration="11" content_type="html">Center for Earth System Science, Tsinghua University, Beijing, China</affiliation>
		<affiliation numeration="12" content_type="html">Department of Environmental Science and Engineering, Tsinghua University, Beijing, China</affiliation>
		<affiliation numeration="13" content_type="html">Department of Geological and Mining Engineering and Sciences and Department of Civil and Environmental Engineering, Michigan Technological University, Houghton, Michigan, USA</affiliation>
		<affiliation numeration="14" content_type="html">now at: Risk Management Solutions, Hackensack, New Jersey, USA</affiliation>
		<affiliation numeration="15" content_type="html">now at: Woodrow Wilson School of Public and International Affairs, Princeton University, Princeton, New Jersey, USA</affiliation>
	</affiliations>
	<abstract content_type="html">We use aircraft observations of carbon monoxide (CO) from the NASA ARCTAS
and NOAA ARCPAC campaigns in April 2008 together with multiyear (2003–2008)
CO satellite data from the AIRS instrument and a global chemical transport
model (GEOS-Chem) to better understand the sources, transport, and
interannual variability of pollution in the Arctic in spring. Model
simulation of the aircraft data gives best estimates of CO emissions in
April 2008 of 26 Tg month&lt;sup&gt;&amp;minus;1&lt;/sup&gt; for Asian anthropogenic, 9.4 for European
anthropogenic, 4.1 for North American anthropogenic, 15 for Russian biomass
burning (anomalously large that year), and 23 for Southeast Asian biomass
burning. We find that Asian anthropogenic emissions are the dominant source
of Arctic CO pollution everywhere except in surface air where European
anthropogenic emissions are of similar importance. Russian biomass burning
makes little contribution to mean CO (reflecting the long CO lifetime) but
makes a large contribution to CO variability in the form of combustion
plumes. Analysis of two pollution events sampled by the aircraft
demonstrates that AIRS can successfully observe pollution transport to the
Arctic in the mid-troposphere. The 2003–2008 record of CO from AIRS shows
that interannual variability averaged over the Arctic cap is very small.
AIRS CO columns over Alaska are highly correlated with the Ocean Niño
Index, suggesting a link between El Niño and Asian pollution transport
to the Arctic. AIRS shows lower-than-average CO columns over Alaska during
April 2008, despite the Russian fires, due to a weakened Aleutian Low
hindering transport from Asia and associated with the moderate 2007–2008 La
Niña. This suggests that Asian pollution influence over the Arctic may
be particularly large under strong El Niño conditions.</abstract>
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</article>

