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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-8-5537-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/5537/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/5537/2008/acpd-8-5537-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/5537/2008/acpd-8-5537-2008.pdf</fulltext_pdf>
	<start_page>5537</start_page>
	<end_page>5561</end_page>
	<publication_date>2008-03-18</publication_date>
	<article_title content_type="html">Source-receptor relationships between East Asian sulfur dioxide emissions and Northern Hemisphere sulfate concentrations</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. Liu</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>D. L. Mauzerall</name>
			<email>mauzeral@princeton.edu</email>
		</author>
		<author numeration="3" affiliations="2">
			<name>L. W. Horowitz</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Woodrow Wilson School of Public and Int. Affairs, Princeton Univ., Princeton, NJ, USA</affiliation>
		<affiliation numeration="2" content_type="html">Geophysical Fluid Dynamics Laboratory, Princeton, NJ, USA</affiliation>
	</affiliations>
	<abstract content_type="html">We analyze the effect of varying East Asian (EA) sulfur emissions on sulfate
concentrations in the Northern Hemisphere, using a global coupled
oxidant-aerosol model (MOZART-2). We conduct a base and five sensitivity
simulations, in which sulfur emissions from each continent are tagged, to
establish the source-receptor (S-R) relationship between EA sulfur emissions
and sulfate concentrations over source and downwind regions. We find that
from west to east across the North Pacific, EA sulfate contributes
approximately 80%&amp;ndash;20% of sulfate at the surface, but at least 50%
at 500 hPa. In addition, EA SO&lt;sub&gt;2&lt;/sub&gt; emissions account for approximately
30%&amp;ndash;50% and 10%&amp;ndash;20% of North American background sulfate over
the western and eastern US, respectively. The contribution of EA sulfate
to the western US at the surface is highest in MAM and JJA, but is lowest
in DJF. Reducing EA SO&lt;sub&gt;2&lt;/sub&gt; emissions will significantly decrease the
spatial extent of the EA sulfate influence over the North Pacific both at
the surface and at 500 mb in all seasons, but the extent of influence is
insensitive to emission increases, particularly in DJF and JJA. We find that
EA sulfate concentrations over most downwind regions respond nearly linearly
to changes in EA SO&lt;sub&gt;2&lt;/sub&gt; emissions, but sulfate concentrations over the EA
source region increase more slowly than SO&lt;sub&gt;2&lt;/sub&gt; emissions, particularly at
the surface and in winter, due to limited availability of oxidants (mostly
H&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;2&lt;/sub&gt;). We find that similar estimates of the S-R relationship for
trans-Pacific transport of EA sulfate would be obtained using either
sensitivity or tagging techniques. Our findings suggest that future changes
in EA sulfur emissions may cause little change in the sulfate induced health
impact over downwind continents but SO&lt;sub&gt;2&lt;/sub&gt; emission reductions may
significantly reduce the sulfate related climate cooling over the North
Pacific and the United States.</abstract>
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</article>

