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<article language="en">
	<journal>
		<journal_title>Geoscientific Model Development Discussions</journal_title>
		<journal_url>www.geosci-model-dev-discuss.net</journal_url>
		<issn>1991-9611</issn>
		<eissn>1991-962X</eissn>
		<volume_number>2</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/gmdd-2-1081-2009</doi>
	<article_url>http://www.geosci-model-dev-discuss.net/2/1081/2009/</article_url>
	<abstract_html>http://www.geosci-model-dev-discuss.net/2/1081/2009/gmdd-2-1081-2009.html</abstract_html>
	<fulltext_pdf>http://www.geosci-model-dev-discuss.net/2/1081/2009/gmdd-2-1081-2009.pdf</fulltext_pdf>
	<start_page>1081</start_page>
	<end_page>1114</end_page>
	<publication_date>2009-07-30</publication_date>
	<article_title content_type="html">Sensitivity of the Community Multiscale Air Quality (CMAQ) Model v4.7 results for the eastern United States to MM5 and WRF meteorological drivers</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>K. W. Appel</name>
			<email>appel.wyat@epa.gov</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>S. J. Roselle</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>R. C. Gilliam</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>J. E. Pleim</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Atmospheric Modeling and Analysis Division, National Exposure Research Laboratory, Office of Research and Development, US Environmental Protection Agency, RTP, NC 27711, USA</affiliation>
	</affiliations>
	<abstract content_type="html">This paper presents a comparison of the operational performances of two
Community Multiscale Air Quality (CMAQ) model v4.7 simulations that utilize
input data from the 5th-generation Mesoscale Model (MM5) and the
Weather Research and Forecasting (WRF) meteorological models. Two sets of
CMAQ model simulations were performed for January and August 2006. One set
utilized MM5 meteorology (MM5-CMAQ) and the other utilized WRF meteorology
(WRF-CMAQ), while all other model inputs and options were kept the same. For
January, predicted ozone (O&lt;sub&gt;3&lt;/sub&gt;) concentrations were higher in the
Southeast and lower Mid-west regions in the WRF-CMAQ simulation, resulting
in slightly higher bias and error as compared to the MM5-CMAQ simulations.
The higher predicted O&lt;sub&gt;3&lt;/sub&gt; concentrations are attributed to less dry
deposition of O&lt;sub&gt;3&lt;/sub&gt; in the WRF-CMAQ simulation due to differences in the
calculation of the vegetation fraction between the MM5 and WRF models. The
WRF-CMAQ results showed better performance for particulate sulfate
(SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2&amp;minus;&lt;/sup&gt;), similar performance for nitrate (NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;minus;&lt;/sup&gt;) and
total nitrate (TNO&lt;sub&gt;3&lt;/sub&gt;), and slightly worse performance for total carbon
(TC) and total fine particulate (PM&lt;sub&gt;2.5&lt;/sub&gt;) mass than the corresponding
MM5-CMAQ results. For August, predictions of O&lt;sub&gt;3&lt;/sub&gt; were notably higher in
the WRF-CMAQ simulation, particularly in the southern United States,
resulting in increased model bias. Concentrations of predicted particulate
SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2&amp;minus;&lt;/sup&gt; were lower in the region surrounding the Ohio Valley and
higher along the Gulf of Mexico in the WRF-CMAQ simulation, contributing to
poorer model performance. The primary cause of the differences in predicted
concentrations between the MM5-CMAQ and WRF-CMAQ simulations is due to
differences in the calculation of the friction velocity (&lt;i&gt;u&lt;/i&gt;&lt;sub&gt;*&lt;/sub&gt;) in MM5 and WRF
models, which has a large effect on the dry deposition of NO, NO&lt;sub&gt;2&lt;/sub&gt; and
HNO&lt;sub&gt;3&lt;/sub&gt;. Differences in the calculation of the vegetation fraction and the
predicted cloud cover, along with several other minor differences in the
simulations also affect the predicted concentrations from CMAQ. The
performance for SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2&amp;minus;&lt;/sup&gt;, NO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;minus;&lt;/sup&gt; and NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt; wet
deposition was similar for both simulations for January and August.</abstract>
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</article>

