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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>7</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/acpd-7-9013-2007</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/7/9013/2007/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/7/9013/2007/acpd-7-9013-2007.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/7/9013/2007/acpd-7-9013-2007.pdf</fulltext_pdf>
	<start_page>9013</start_page>
	<end_page>9051</end_page>
	<publication_date>2007-06-26</publication_date>
	<article_title content_type="html">Intercontinental transport of pollution and dust aerosols: implications for regional air quality</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>Mian Chin</name>
			<email>mian.chin@nasa.gov</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>T. Diehl</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>P. Ginoux</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>W. Malm</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">NASA Goddard Space Flight Center, Greenbelt, MD, USA</affiliation>
		<affiliation numeration="2" content_type="html">University of Maryland Baltimore County, Baltimore, MD, USA</affiliation>
		<affiliation numeration="3" content_type="html">NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ, USA</affiliation>
		<affiliation numeration="4" content_type="html">National Parck Service, CIRA, Colorado State University, Fort Collins, CO, USA</affiliation>
	</affiliations>
	<abstract content_type="html">We use the global model GOCART to examine the impact of pollution and dust
aerosols emitted from their major sources on surface fine particulate matter
concentrations at regional and hemispheric scales. Focusing on the North
America region in 2001, we use measurements from the IMPROVE network in the
United States to evaluate the model-simulated surface concentrations of the
&quot;reconstructed fine mass&quot; (RCFM) and its components of ammonium sulfate,
black carbon (BC), organic matter (OM), and fine mode dust. We then quantify
the RCFM budget in terms of the RCFM composition, type, and origin to find
that in the eastern U.S., ammonium sulfate is the dominant RCFM component
(~60%) whereas in the western U.S., dust and OM are just as
important as sulfate but have considerable seasonal variations, especially
in the NW. On an annual average, North America regional pollution accounts
for nearly 30&amp;ndash;40% of the surface RCFM in the western U.S., and for a
much higher proportion of 65&amp;ndash;70% in the eastern U.S. By contrast,
pollution from outside of North America contributes to just 2&amp;ndash;6%
(~0.2 μg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;) of the total RCFM over the U.S. on an annual
average. In comparison, long-range transport of dust is more efficient than
that of pollution, which brings 3 to 4 times more fine particles to the U.S.
(0.5&amp;ndash;0.8 μg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; on an annual average) with a maximum influence
in spring and over the NW. Of the major pollution regions, Europe has the
largest potential to affect the surface aerosol concentrations in other
continents due to its shorter distance from receptor continents and its
larger fraction of sulfate-producing precursor gas in the outflow. With the
IPCC emission scenario for the year 2000, we find that European emissions
increase levels of ammonium sulfate by 1&amp;ndash;5 μg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; over the
surface of northern Africa and western Asia, and its contribution to eastern
Asia (&amp;ge;0.2 μg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;) is twice as much as the Asian
contribution to North America. Asia and North America pollution emissions
exert strong impacts on their neighboring oceans, but their influences on
other continents are relatively small (&amp;le;10%) due to the long
traveling distance across the oceans and efficient removal during transport.
Among the major dust source regions, Asia displays a significant influence
over large areas in the Northern Hemisphere except over the North Atlantic
and the tropics, where African dust dominates. The trans-Pacific transport
of Asian dust is much more efficient than that of Asian pollution because of
the higher elevation and lower removal rate of dust. We notice that the
African dust can travel eastward through a pathway spanning across Asia and
North Pacific to settle down over the surface of western North America.
African dust transported through such a pathway is difficult to detect
because it usually merges and travels together with the Asian dust.</abstract>
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