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<article language="en">
	<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>3</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2007</publication_year>
	</journal>
	<doi>10.5194/cp-3-89-2007</doi>
	<article_url>http://www.clim-past.net/3/89/2007/</article_url>
	<abstract_html>http://www.clim-past.net/3/89/2007/cp-3-89-2007.html</abstract_html>
	<fulltext_pdf>http://www.clim-past.net/3/89/2007/cp-3-89-2007.pdf</fulltext_pdf>
	<start_page>89</start_page>
	<end_page>95</end_page>
	<publication_date>2007-02-07</publication_date>
	<article_title content_type="html">Summer temperature trend over the past two millennia using air content in Himalayan ice</article_title>
	<authors>
		<author numeration="1" affiliations="1,2,3">
			<name>S. Hou</name>
			<email>shugui@lzb.ac.cn</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. Chappellaz</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>J. Jouzel</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>P. C. Chu</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>V. Masson-Delmotte</name>
		</author>
		<author numeration="6" affiliations="3">
			<name>D. Qin</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>D. Raynaud</name>
		</author>
		<author numeration="8" affiliations="5">
			<name>P. A. Mayewski</name>
		</author>
		<author numeration="9" affiliations="6">
			<name>V. Y. Lipenkov</name>
		</author>
		<author numeration="10" affiliations="3">
			<name>S. Kang</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Lab. de Glaciologie et Geophysique de l&apos;Environnement (CNRS-UJF), 54 rue Molière, Domaine Univ., BP 96, 38402 St Martin d&apos;Hères, France</affiliation>
		<affiliation numeration="2" content_type="html">IPSL-Lab. des Sciences du Climat et de l&apos;Environnement (CEA-CNRS-UVSQ), CE Saclay, Annexe Orme des Merisiers, 91191 Gif-sur-Yvette, France</affiliation>
		<affiliation numeration="3" content_type="html">Lab. of Cryosphere and Environment, Chinese Academy of Sciences, 260 Donggang West Road, 730000 Lanzhou, China</affiliation>
		<affiliation numeration="4" content_type="html">Naval Ocean-Atmosphere Prediction Lab., Dept. of Oceanography, Naval Postgraduate School, Monterey, CA 93943, USA</affiliation>
		<affiliation numeration="5" content_type="html">Climate Change Institute (CCI), Univ. of Maine, Orono, ME 04469, USA</affiliation>
		<affiliation numeration="6" content_type="html">Arctic and Antarctic Research Institute, Beringa Street 38, 199397, St. Petersburg, Russia</affiliation>
	</affiliations>
	<abstract content_type="html">Two Himalayan ice cores display a factor-two decreasing trend of air content
over the past two millennia, in contrast to the relatively stable values in
Greenland and Antarctica ice cores over the same period. Because the air
content can be related with the relative frequency and intensity of melt
phenomena, its variations along the Himalayan ice cores provide an
indication of summer temperature trend. Our reconstruction point toward an
unprecedented warming trend in the 20th century but does not depict the
usual trends associated with &quot;Medieval Warm Period&quot; (MWP), or &quot;Little Ice
Age&quot; (LIA).</abstract>
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</article>

