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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>14</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/hess-14-481-2010</doi>
	<article_url>http://www.hydrol-earth-syst-sci.net/14/481/2010/</article_url>
	<abstract_html>http://www.hydrol-earth-syst-sci.net/14/481/2010/hess-14-481-2010.html</abstract_html>
	<fulltext_pdf>http://www.hydrol-earth-syst-sci.net/14/481/2010/hess-14-481-2010.pdf</fulltext_pdf>
	<start_page>481</start_page>
	<end_page>489</end_page>
	<publication_date>2010-03-12</publication_date>
	<article_title content_type="html">Growth of a high-elevation large inland lake, associated with climate change and permafrost degradation in Tibet</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. Liu</name>
			<email>jsliu@itpcas.ac.cn</email>
		</author>
		<author numeration="2" affiliations="1,3">
			<name>S. Kang</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>T. Gong</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>A. Lu</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Nam Co Monitoring and Research Station for Multisphere Interaction, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China</affiliation>
		<affiliation numeration="2" content_type="html">Hydrology and Water Resources Bureau of Tibet, Lhasa 850000, China</affiliation>
		<affiliation numeration="3" content_type="html">Key Laboratory of Cryosphere and Environment, Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences, Lanzhou 730000, China</affiliation>
	</affiliations>
	<abstract content_type="html">This study analyzed satellite images and long term climate variables from a
high-elevation meteorological station (4730 m) and streamflow records to
examine hydrological response of Nam Co Lake (4718 m), the largest lake on
the Tibetan Plateau, over the last 50 years. The results show the lake area
extended by 51.8 km&lt;sup&gt;2&lt;/sup&gt; (2.7% of the total area) when compared with
the area in 1976. This change is associated with an annual precipitation
increase of 65 mm (18.6%), annual and winter mean temperature increases
of 0.9 &amp;deg;C and 2.1 &amp;deg;C respectively, an annual runoff increase of 20%
and an annual pan evaporation decrease of about 2%, during the past 20 years.
The year of the change point in annual precipitation, air
temperature, annual pan evaporation and runoff occurred in 1971, 1983, 1997
and 1997, respectively. The timing of the lake growth corresponds with the
abrupt increase in annual precipitation and runoff since the mid-1990s.</abstract>
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</article>

