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<article language="en">
	<journal>
		<journal_title>Hydrology and Earth System Sciences</journal_title>
		<journal_url>www.hydrol-earth-syst-sci.net</journal_url>
		<issn>1027-5606</issn>
		<eissn>1607-7938</eissn>
		<volume_number>13</volume_number>
		<issue_number>11</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/hess-13-2023-2009</doi>
	<article_url>http://www.hydrol-earth-syst-sci.net/13/2023/2009/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci.net/13/2023/2009/hess-13-2023-2009.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci.net/13/2023/2009/hess-13-2023-2009.pdf</fulltext_pdf>
	<start_page>2023</start_page>
	<end_page>2030</end_page>
	<publication_date>2009-11-02</publication_date>
	<article_title content_type="html">Snow distribution over the Namco lake area of the Tibetan Plateau</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Li</name>
			<email>mshli@lzb.ac.cn</email>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>Y. Ma</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>Z. Hu</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>H. Ishikawa</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>Y. Oku</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Cold and Arid Region Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China</affiliation>
		<affiliation numeration="3" content_type="html">Disaster Prevention Research Institute, Kyoto University, Kyoto 611-0011, Japan</affiliation>
	</affiliations>
	<abstract content_type="html">The mesoscale snow distribution over the Namco lake area of the
Tibetan Plateau on October 2005 has been investigated in this paper.
The base and revised experiments were conducted using the Weather
Research Model (WRF) with three nested grids that included a 1 km
finest grid centered on the Namco station. Our simulation ran from
6 October through to 10 October 2005, which was concurrent with long
term meteorological observations. Evaluation against boundary layer
meteorological tower measurements and flux observations showed that
the model captured the observed 2 m temperature and 10 m winds
reasonably well in the revised experiment. The results suggest that
output snow depth maximum amounts from two simulated experiments
were centered downwind of the Namco lakeshore. Modified surface
state variable, for example, surface skin temperature on the lake
help to increase simulated credibility.</abstract>
	<references>
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</article>

