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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>9</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-7079-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/7079/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/7079/2009/acpd-9-7079-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/7079/2009/acpd-9-7079-2009.pdf</fulltext_pdf>
	<start_page>7079</start_page>
	<end_page>7113</end_page>
	<publication_date>2009-03-16</publication_date>
	<article_title content_type="html">Effect of regional precursor emission controls on long-range ozone  transport – Part 2: steady-state changes in ozone air quality and impacts on human mortality</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. J. West</name>
			<email>jasonwest@unc.edu</email>
		</author>
		<author numeration="2" affiliations="2,4">
			<name>V. Naik</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>L. W. Horowitz</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>A. M. Fiore</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">University of North Carolina, Chapel Hill, NC, USA</affiliation>
		<affiliation numeration="2" content_type="html">Princeton University, Princeton, NJ, USA</affiliation>
		<affiliation numeration="3" content_type="html">NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ, USA</affiliation>
		<affiliation numeration="4" content_type="html">now at: ATMOS Research and Consulting, Lubbock, TX, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Large-scale changes in ozone precursor emissions affect ozone directly in
the short term, and also affect methane, which in turn causes long-term
changes in ozone that affect surface ozone air quality. Here we assess the
effects of changes in ozone precursor emissions on the long-term change in
surface ozone via methane, as a function of the emission region, by modeling
10% reductions in anthropogenic nitrogen oxide (NO&lt;sub&gt;x&lt;/sub&gt;) emissions from
each of nine world regions. Reductions in NO&lt;sub&gt;x&lt;/sub&gt; emissions from all world
regions increase methane and long-term surface ozone. While this long-term
increase is small compared to the intra-regional short-term ozone decrease,
it is comparable to or larger than the short-term inter-continental ozone
decrease for some source-receptor pairs. The increase in methane and
long-term surface ozone per ton of NO&lt;sub&gt;x&lt;/sub&gt; reduced is greatest in tropical
and Southern Hemisphere regions, exceeding that from temperate Northern
Hemisphere regions by roughly a factor of ten. We also assess changes in
premature ozone-related human mortality associated with regional precursor
reductions and long-range transport, showing that for 10% regional
NO&lt;sub&gt;x&lt;/sub&gt; reductions, the strongest inter-regional influence is for emissions
from Europe affecting mortalities in Africa. Reductions of NO&lt;sub&gt;x&lt;/sub&gt; in North
America, Europe, the Former Soviet Union, and Australia are shown to reduce
more mortalities outside of the source regions than within. Among world
regions, NO&lt;sub&gt;x&lt;/sub&gt; reductions in India cause the greatest number of avoided
mortalities per ton, mainly in India itself. Finally, by increasing global
methane, NO&lt;sub&gt;x&lt;/sub&gt; reductions in one hemisphere tend to cause long-term
increases in ozone concentration and mortalities in the opposite hemisphere.
Reducing emissions of methane, and to a lesser extent carbon monoxide and
non-methane volatile organic compounds, alongside NO&lt;sub&gt;x&lt;/sub&gt; reductions would
avoid this disbenefit.</abstract>
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</article>

