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	<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>9</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-21285-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/21285/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/21285/2009/acpd-9-21285-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/21285/2009/acpd-9-21285-2009.pdf</fulltext_pdf>
	<start_page>21285</start_page>
	<end_page>21315</end_page>
	<publication_date>2009-10-09</publication_date>
	<article_title content_type="html">Estimating mercury emission outflow from East Asia using CMAQ-Hg</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>C.-J. Lin</name>
			<email>jerry.lin@lamar.edu</email>
		</author>
		<author numeration="2" affiliations="3">
			<name>L. Pan</name>
		</author>
		<author numeration="3" affiliations="4">
			<name>D. G. Streets</name>
		</author>
		<author numeration="4" affiliations="5">
			<name>S. K. Shetty</name>
		</author>
		<author numeration="5" affiliations="6">
			<name>C. Jang</name>
		</author>
		<author numeration="6" affiliations="7">
			<name>X. Feng</name>
		</author>
		<author numeration="7" affiliations="3">
			<name>H.-W. Chu</name>
		</author>
		<author numeration="8" affiliations="5">
			<name>T. C. Ho</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Civil Engineering, Lamar University, Beaumont, TX 77710, USA</affiliation>
		<affiliation numeration="2" content_type="html">School of Environmental Science &amp; Engineering, South China University of Technology, Guangzhou, 510006, Guangdong, China</affiliation>
		<affiliation numeration="3" content_type="html">Department of Mechanical Engineering, Lamar University, Beaumont, TX 77710, USA</affiliation>
		<affiliation numeration="4" content_type="html">Decision and Information Sciences Division, Argonne National Laboratory, Argonne, IL 60439, USA</affiliation>
		<affiliation numeration="5" content_type="html">Department of Chemical Engineering, Lamar University, Beaumont, TX 77710, USA</affiliation>
		<affiliation numeration="6" content_type="html">Office of Air Quality Planning and Standards, USEPA, Research Triangle Park, NC 27711, USA</affiliation>
		<affiliation numeration="7" content_type="html">State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China</affiliation>
	</affiliations>
	<abstract content_type="html">East Asia contributes nearly 50% of the global
anthropogenic mercury emissions into the atmosphere. Recently,
there are concerns for the long-range transport of mercury
from East Asia to North America, which may lead to enhanced
dry and wet depositions in North America. In this study, we
performed four monthly simulations (January, April, July and
October in 2005) using CMAQ-Hg v4.6 in an East Asian model
domain. Coupled with a mass balance analysis and a number of
emission inventory scenarios, the chemical transport of
atmospheric mercury, the seasonal mercury transport budgets
and mercury emission outflow from the East Asian region were
investigated. The total annual mercury deposition in the
region for the modeling year is estimated to be 821 Mg, with
396 Mg contributed by wet deposition and 425 Mg contributed
by dry deposition. Regional mercury transport budgets show
strong seasonal variability, with a net removal of RGM
(7~5 Mg mo&lt;sup&gt;&amp;minus;1&lt;/sup&gt;) and PHg (13~21 Mg mo&lt;sup&gt;&amp;minus;1&lt;/sup&gt;), and
a net export of GEM (60~130 Mg mo&lt;sup&gt;&amp;minus;1&lt;/sup&gt;) from the study
domain. The annual outflow caused by the East Asian emission
is estimated to be in the range of
1369~1671 Mg yr&lt;sup&gt;&amp;minus;1&lt;/sup&gt;, primarily in the form of
GEM. This represents about 75% of the total mercury
emissions (anthropogenic and natural) in the region. The
emission outflow from this source region would contribute
to 20~30% of mercury deposition in areas remote
from anthropogenic emission sources.</abstract>
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