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<article language="en">
	<journal>
		<journal_title>Climate of the Past Discussions</journal_title>
		<journal_url>www.clim-past-discuss.net</journal_url>
		<issn>1814-9340</issn>
		<eissn>1814-9359</eissn>
		<volume_number>3</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/cpd-3-655-2007</doi>
	<article_url>http://www.clim-past-discuss.net/3/655/2007/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/3/655/2007/cpd-3-655-2007.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/3/655/2007/cpd-3-655-2007.pdf</fulltext_pdf>
	<start_page>655</start_page>
	<end_page>678</end_page>
	<publication_date>2007-03-23</publication_date>
	<article_title content_type="html">The LGM surface climate and atmospheric circulation over East Asia and the North Pacific in the PMIP2 coupled model simulations</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>W. Yanase</name>
			<email>yanase@ccsr.u-tokyo.ac.jp</email>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>A. Abe-Ouchi</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Center for Climate System Research, The University of Tokyo</affiliation>
		<affiliation numeration="2" content_type="html">Frontier Research Center for Global Change, Japan Agency for Marine-Earth Science and Technology</affiliation>
	</affiliations>
	<abstract content_type="html">The surface climate and atmospheric circulation
over East Asia and the North Pacific
at the last glacial maximum has been investigated
using the outputs from several coupled atmosphere-ocean
general circulation model in PMIP2 database.
In boreal summer, the weakening of high pressure over the North Pacific
and less precipitation over East Asia are analyzed in most models.
The reduced moisture transport seems to
result in the less precipitation over East Asia.
In boreal winter, the intensification of the Aleutian low and southward shift
of the upper-level jet are analyzed in most models.
Some of these results are consistent with geological records
such as pollen, lake status and dust transport.</abstract>
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</article>

