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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>8</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-14765-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/14765/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/14765/2008/acpd-8-14765-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/14765/2008/acpd-8-14765-2008.pdf</fulltext_pdf>
	<start_page>14765</start_page>
	<end_page>14817</end_page>
	<publication_date>2008-08-01</publication_date>
	<article_title content_type="html">Coupling aerosol-cloud-radiative processes in the WRF-Chem model: investigating the radiative impact of elevated point sources</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>E. G. Chapman</name>
			<email>elaine.chapman@pnl.gov</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>W. I. Gustafson, Jr.</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>R. C. Easter</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>J. C. Barnard</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>S. J. Ghan</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>M. S. Pekour</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>J. D. Fast</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Pacific Northwest National Laboratory, P.O. Box 999, Richland, Washington D.C. 99352, USA</affiliation>
	</affiliations>
	<abstract content_type="html">The local and regional influence of elevated point sources on summertime
aerosol forcing and cloud-aerosol interactions in northeastern North America
was investigated using the WRF-Chem community model. The direct effects of
aerosols on incoming solar radiation were simulated using existing modules
to relate aerosol sizes and chemical composition to aerosol optical
properties. Indirect effects were simulated by adding a prognostic treatment
of cloud droplet number and adding modules that activate aerosol particles
to form cloud droplets, simulate aqueous-phase chemistry, and tie a
two-moment treatment of cloud water (cloud water mass and cloud droplet
number) to an existing radiation scheme. Fully interactive feedbacks thus
were created within the modified model, with aerosols affecting cloud
droplet number and cloud radiative properties, and clouds altering aerosol
size and composition via aqueous processes, wet scavenging, and
gas-phase-related photolytic processes. Comparisons of a baseline simulation
with observations show that the model captured the general temporal cycle of
aerosol optical depths (AODs) and produced clouds of comparable thickness to
observations at approximately the proper times and places. The model
overpredicted SO&lt;sub&gt;2&lt;/sub&gt; mixing ratios and PM&lt;sub&gt;2.5&lt;/sub&gt; mass, but reproduced the
range of observed SO&lt;sub&gt;2&lt;/sub&gt; to sulfate aerosol ratios, suggesting that
atmospheric oxidation processes leading to aerosol sulfate formation are
captured in the model. The baseline simulation was compared to a sensitivity
simulation in which all emissions at model levels above the surface layer
were set to zero, thus removing stack emissions. Instantaneous,
site-specific differences for aerosol and cloud related properties between
the two simulations could be quite large, as removing above-surface emission
sources influenced when and where clouds formed within the modeling domain.
When summed spatially over the finest resolution model domain (the extent of
which corresponds to the typical size of a single GCM grid cell) and
temporally over a three day analysis period, total rainfall in the
sensitivity simulation increased by 31% over that in the baseline
simulation. Fewer optically thin clouds, arbitrarily defined as a cloud
exhibiting an optical depth less than 1, formed in the sensitivity
simulation. Domain-averaged AODs dropped from 0.46 in the baseline
simulation to 0.38 in the sensitivity simulation. The overall net effect of
additional aerosols attributable to primary particulates and aerosol
precursors from point source emissions above the surface was a
domain-averaged reduction of 5 W m&lt;sup&gt;&amp;minus;2&lt;/sup&gt; in mean daytime downwelling
shortwave radiation.</abstract>
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