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	<journal>
		<journal_title>Climate of the Past</journal_title>
		<journal_url>www.clim-past.net</journal_url>
		<issn>1814-9324</issn>
		<eissn>1814-9332</eissn>
		<volume_number>7</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2011</publication_year>
	</journal>
	<doi>10.5194/cp-7-685-2011</doi>
	<article_url>http://www.clim-past.net/7/685/2011/</article_url>
	<abstract_html>http://www.clim-past.net/7/685/2011/cp-7-685-2011.html</abstract_html>
	<fulltext_pdf>http://www.clim-past.net/7/685/2011/cp-7-685-2011.pdf</fulltext_pdf>
	<start_page>685</start_page>
	<end_page>692</end_page>
	<publication_date>2011-07-04</publication_date>
	<article_title content_type="html">Climate patterns in north central China during the last 1800 yr and their possible driving force</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>L. Tan</name>
			<email>tanlch@ieecas.cn</email>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>Y. Cai</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>Z. An</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>L. Yi</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>H. Zhang</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>S. Qin</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS, Xi&apos;an, 710075, China</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Global Environmental Change, Xi&apos;an Jiaotong University, Xi&apos;an, 710049, China</affiliation>
		<affiliation numeration="3" content_type="html">Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, SOA, Qingdao, 266061, China</affiliation>
	</affiliations>
	<abstract content_type="html">We synthesized high-resolution precisely-dated stalagmite
records and historical document records from north central China to
reconstruct a decadal resolution precipitation record during the last 1800
years (190–1980 AD). The synthesized precipitation record shows coincident
variations and significant positive correlations with the temperature
reconstructions on centennial- to multidecadal-scale, suggesting
warm-humid/cool-dry was the main climate pattern in north central China over
the past 1800 years. Solar activity may be the dominant force that drove the
same-phase variations of the temperature and precipitation in north central
China.</abstract>
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</article>

