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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>6</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/acpd-7-15565-2007</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/7/15565/2007/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/7/15565/2007/acpd-7-15565-2007.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/7/15565/2007/acpd-7-15565-2007.pdf</fulltext_pdf>
	<start_page>15565</start_page>
	<end_page>15580</end_page>
	<publication_date>2007-11-05</publication_date>
	<article_title content_type="html">Dust aerosol radiative effect and influence on urban atmospheric boundary layer</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>L. Zhang</name>
			<email>zhanglei@lzu.edu.cn</email>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>M. Chen</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>L. Li</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">College of Atmospheric Sciences, Lanzhou University, Lanzhou, 730000, China</affiliation>
		<affiliation numeration="2" content_type="html">Key Laboratory of Western China&apos;s Environmental Systems (Ministry of Education), Lanzhou University, Lanzhou, 730000, China</affiliation>
		<affiliation numeration="3" content_type="html">Beijing Regional Climate Center, Beijing Meteorological Bureau, Beijing, 100089, China</affiliation>
	</affiliations>
	<abstract content_type="html">An 1.5-level-closure and 3-D non-stationary atmospheric boundary layer (ABL)
model and a radiation transfer model with the output of Weather Research and
Forecast (WRF) Model and lidar AML-1 are employed to simulate the dust
aerosol radiative effect and its influence on ABL in Beijing for the period
of 23&amp;ndash;26 January 2002 when a dust storm occurred. The simulation shows that
daytime dust aerosol radiative effect heats up the ABL at the mean rate of
about 0.68 K/h. The horizontal wind speed from ground to 900 m layer is also
overall increased, and the value changes about 0.01 m/s at 14:00 LT near the
ground. At night, the dust aerosol radiative effect cools the ABL at the
mean rate of &amp;minus;0.21 K/h and the wind speed lowers down at about &amp;minus;0.19 m/s at
02:00 LT near the ground.</abstract>
	<references>
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</article>

