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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-7-6487-2007</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/7/6487/2007/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/7/6487/2007/acpd-7-6487-2007.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/7/6487/2007/acpd-7-6487-2007.pdf</fulltext_pdf>
	<start_page>6487</start_page>
	<end_page>6525</end_page>
	<publication_date>2007-05-14</publication_date>
	<article_title content_type="html">Sensitivity of PM&lt;sub&gt;2.5&lt;/sub&gt; to climate in the Eastern U.S.: a modeling case study</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. P. Dawson</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>P. J. Adams</name>
		</author>
		<author numeration="3" affiliations="1,2">
			<name>S. N. Pandis</name>
			<email>spyros@andrew.cmu.edu</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Carnegie Mellon University, Pittsburgh, Pennsylvania, USA</affiliation>
		<affiliation numeration="2" content_type="html">University of Patras, Patra, Greece</affiliation>
	</affiliations>
	<abstract content_type="html">The effects of various meteorological parameters on PM&lt;sub&gt;2.5&lt;/sub&gt;
concentrations in the Eastern US are examined using the PMCAMx chemical
transport model. A suite of perturbations in temperature, wind speed,
absolute humidity, mixing height, cloud cover, and precipitation are imposed
on base case conditions corresponding to periods in July 2001 and January
2002 in order to determine the sensitivities of PM&lt;sub&gt;2.5&lt;/sub&gt; concentrations
and composition to these meteorological parameters. Temperature had a major
effect on average PM&lt;sub&gt;2.5&lt;/sub&gt; in January (&amp;ndash;170 ng m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; K&lt;sup&gt;&amp;minus;1&lt;/sup&gt;) due
largely to the evaporation of ammonium nitrate and organic aerosol at higher
temperatures; increases in sulfate production with increased temperature
counteracted much of this decrease in July. Changes in mixing height also
had major effects on PM&lt;sub&gt;2.5&lt;/sub&gt; concentrations: 73 ng m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; (100 m)&lt;sup&gt;&amp;minus;1&lt;/sup&gt; in January and 210 ng m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; (100 m)&lt;sup&gt;&amp;minus;1&lt;/sup&gt; in July. Changes in
wind speed (30 to 55 ng m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; %&lt;sup&gt;&amp;minus;1&lt;/sup&gt;) and absolute humidity (15 to
20 ng m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; %&lt;sup&gt;&amp;minus;1&lt;/sup&gt;) also had appreciable effects on average
PM&lt;sub&gt;2.5&lt;/sub&gt; concentrations. Precipitation changes had large impacts on parts
of the domain (a consequence of the base case meteorology), with
sensitivities to changing area of precipitation in July up to 100 ng m&lt;sup&gt;&amp;minus;3&lt;/sup&gt; %&lt;sup&gt;&amp;minus;1&lt;/sup&gt;. Perturbations in cloud cover had the smallest effects
on average PM&lt;sub&gt;2.5&lt;/sub&gt; concentrations. The changes in PM&lt;sub&gt;2.5&lt;/sub&gt;
concentrations resulting from changing all eight meteorological parameters
simultaneously were approximated within 25% or so by summing the changes
that resulted when the eight perturbations were imposed separately. The
sensitivities of PM&lt;sub&gt;2.5&lt;/sub&gt; concentrations to changes in these
meteorological parameters indicate that changes in climate may have
important impacts on PM&lt;sub&gt;2.5&lt;/sub&gt; concentrations.</abstract>
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