<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.clim-past.net/inc/cp/copernicus.dtd">
<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>4</volume_number>
		<issue_number>3</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/cp-4-175-2008</doi>
	<article_url>http://www.clim-past.net/4/175/2008/</article_url>
	<abstract_html>http://www.clim-past.net/4/175/2008/cp-4-175-2008.html</abstract_html>
	<fulltext_pdf>http://www.clim-past.net/4/175/2008/cp-4-175-2008.pdf</fulltext_pdf>
	<start_page>175</start_page>
	<end_page>180</end_page>
	<publication_date>2008-08-22</publication_date>
	<article_title content_type="html">Precipitation record since AD 1600 from ice cores on the central Tibetan Plateau</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>T. Yao</name>
			<email>tdyao@itpcas.ac.cn</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>K. Duan</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>B. Xu</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>N. Wang</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>X. Guo</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>X. Yang</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100085, China</affiliation>
		<affiliation numeration="2" content_type="html">State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Engineering and Environment Research Institute, CAS, Lanzhou, Gansu, 730000, China</affiliation>
	</affiliations>
	<abstract content_type="html">Lack of reliable long-term precipitation record from the northern Tibetan
Plateau has constrained our understanding of precipitation variations in
this region. We drilled an ice core on the Puruogangri Ice Field in the
central Tibetan Plateau in 2000 to reveal the precipitation variations. The
well dated part of the core extends back to AD 1600, allowing us to
construct a 400-year annual accumulation record. This record shows that the
central Tibetan plateau experienced a drier period with an average annual
precipitation of ~300 mm in the 19th century, compared to ~450 mm
in the wetter periods during 1700–1780 and the 20th century.
This pattern agrees with precipitation reconstructions from the Dunde and
Guliya ice cores on the northern Plateau but differs from that found in the
Dasuopu ice cores from the southern Plateau The north-south contrasts in
precipitation reconstruction reveals difference in moisture origin between
the south Tibetan Plateau dominated by the Asian monsoon and the north
Tibetan Plateau dominated by the continental recycling and the westerlies.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Achim, B. and Mantwill, B.: Summer temperature and summer monsoon history on the Tibetan plateau during the last 400 years recorded by tree rings, Geophys. Res. Lett., 31, 24 205, doi:10.1029/2004GL020793, 2004. </reference>
		<reference numeration="2" content_type="text"> Bolzan, J. F.: Ice flow at the dome-c ice divide based on a deep temperature profile, J. Geophys. Res., 90(D5), 8111–8124, 1985. </reference>
		<reference numeration="3" content_type="text"> Davis, M. E., Thompson, L. G., Yao, T., and Wang, N.: Forcing of the Asian monsoon on the Tibetan Plateau: Evidence from high-resolution ice core and tropical coral records, J. Geophys. Res., 110, D04101, doi:10.1029/2004JD004933, 2005. </reference>
		<reference numeration="4" content_type="text"> Duan, K., Wang, N., and Pu, J.: Indian Monsoon Abrupt Change recorded in Dasuopu ice core, Chinese Sci. B., 46(24), 2069–2073, 2001 (in Chinese). </reference>
		<reference numeration="5" content_type="text"> Duan, K. and Yao, T.: Correspondence of monsoonal precipitation recorded in Himalayan glacier accumulation to warming, Chinese Sci. B., 47(19), 1508–1511, 2002 (in Chinese). </reference>
		<reference numeration="6" content_type="text"> Gao, Y., Arimoto, R., Zhou, M., Merrill, J., and Duce, R. A.: Relationships between the dust concentration over eastern Asian and the remote North Pacific, J. Geophys. Res., 97, 9867–9872, 1992. </reference>
		<reference numeration="7" content_type="text"> Hardy, D. R., Vuille, M., and Bradley, R. S.: Variability of snow accumulation and isotopic composition on Nevado Sajama, Bolivia, J. Geophys. Res., 108, D22, doi:10.1029/2003JD003623, 2003. </reference>
		<reference numeration="8" content_type="text"> Hulme, M., Mitchell, J., Ingram, W., Lowe, J., Johns, T., New, M., and Viner, D.: Climate change scenarios for global impacts studies, Global Environ. Change, 9, Supplement 1, S3–S19, 1999. </reference>
		<reference numeration="9" content_type="text"> Hulme, M.: Validation of large-scale precipitation fields in General Circulation Models, in: Global Precipitation and Climate Change, edited by: Desbois, M. and Desalmand, F., Springer, Berlin, 387–405, 1994. </reference>
		<reference numeration="10" content_type="text"> Husar, R. B., Tratt, D. M., Schichtel, B. A., Falke, S. R., Li, F., Jaffe, D., Gasso, S., Gill, T., Laulainen, N. S., Lu, F., Reheis, M. C., Chun, Y., Westphal, D., Holben, B. N., Gueymard, C., McKendry, I., Kuring, N., Feldman, G. C., McClain, C., Frouin, R. J., Merrill, J., Dubois, D., Vignola, F., Murayama, T., Nicklovic, S., Wilson, W. E., Sassen, K., Sugimoto, N., and Malm, W. C.: The Asian dust events of April 1998, J. Geophys. Res, 106(D16), 18 317–18 330, 2001. </reference>
		<reference numeration="11" content_type="text"> Kotlyakov, V. M., Grosswald, M. G., Dyurgerov, M. B., and Mazo, V. L.: The reaction of glaciers to impending climate change, Polar Geogr. Ecol., 15(3), 203–217, 1991. </reference>
		<reference numeration="12" content_type="text"> Liu, X. and Hou, P.: Summer precipitation variation on east-central Plateau and its correlation with NAO, Meteorol. B., 57(5), 561–570, 1999 (in Chinese). </reference>
		<reference numeration="13" content_type="text"> Nitta, T. and Hu, Z. Z.: Summer climate variability in China and its association with 500 hPa height and tropical convection, J. Meteorol. Soc., Japan, 74, 425–445, 1996. </reference>
		<reference numeration="14" content_type="text"> Oerlemans, J. and Fortuin, J. P. F.: Sensitivity of glaciers and small ice caps to greenhouse warming, Science, 258, 115–118, 1992. </reference>
		<reference numeration="15" content_type="text"> Pu, J., Yao, T., Wang, N., Ding, L., and Zhang, Q.: Puruogangri ice field and its variations since the Little Ice Age of the Northern Tibetan Plateau, J. Glaciol. Geocryol., 24(1), 87–92, 2002 (in Chinese). </reference>
		<reference numeration="16" content_type="text"> Reeh, N.: A flow-line model for calculating the surface profile and the velocity, strain-rate, and stress-fields in an ice-sheet, J. Glaciol., 34(116), 46–54, 1988. </reference>
		<reference numeration="17" content_type="text"> Shao, X., Huang, L., and Liu, H.: Tree ring recorded millennial precipitation change in Delingha, Qinghai, Sci. China. Ser. D, 349(2), 145–153, 2004 (in Chinese). </reference>
		<reference numeration="18" content_type="text"> Sheppard, P. R., Tarasov, P. E., Graumlich, L. J., Heussner, K. U., Wagner, M., Oesterle, H., and Thompson, L. G.: Annual precipitation since 515 BC reconstructed from living and fossil juniper growth of northeastern Qinghai Province, China. Clim. Dynam., 23, 869–881, 2004. </reference>
		<reference numeration="19" content_type="text"> Thompson, L. G., Davis, M. E., Mosley-Thompson, E., Sowers, T. A., Henderson, K. A., Zagorodnov, V. S., Lin, P.-N., Mikhalenko, V. N., Campen, R. K., Bolzan, J. F., Cole-Dai, J., and Francou, B.: A 25,000-Year Tropical Climate History from Bolivian Ice Cores, Science, 282(5395), 1858–1864, doi:10.1126/science.282.5395.1858, 1998. </reference>
		<reference numeration="20" content_type="text"> Thompson, L. G., Mosley-Thompson, E., Dansgaard, W., Grootes, P. M.: The Little Ice Age as Recorded in the Stratigraphy of the Tropical Quelccaya Ice Cap, Science, 234(4774), 361–364, doi:10.1126/science.234.4774.361, 1986. </reference>
		<reference numeration="21" content_type="text"> Thompson, L. G., Yao T., Davis, M. E., Mosley-Thompson, E., Mashiotta, T. A., Lin, P., Mikhalenko, V. N., and Zagorodnov, V. S.: Holocene climate variability archived in the Puruogangri ice cap on the central Tibetan Plateau, Ann. Glaciol., 43, 61–69, 2006. </reference>
		<reference numeration="22" content_type="text"> Yao, T.: Abrupt Climate Change on the Tibetan Plateau in LGM – comparison between Guliya ice core and GRIP (in Chinese), Sci. China. Ser. D, 29(2), 175–184, 1999. </reference>
		<reference numeration="23" content_type="text"> Yao, T.: Discovery of the Puruogangri Ice Field on central Plateau and its scientific significance, J. Glaciol. Geocryol., 22(1), 1–2, 2000 (in Chinese). </reference>
		<reference numeration="24" content_type="text"> Yao, T., Duan, K., Tian, L., and Sun, W.: Dasuopu ice core accumulation record and Indian summer monsoonal precipitation change in the past 400a, Sci. China. Ser. D, 30(6), 619–627, 2000 (in Chinese). </reference>
		<reference numeration="25" content_type="text"> Yao, T. and Jiao, K.: Climate change since Little Ice Age recorded in the Guliya ice core, Sci. China. Ser. B, 25(10), 1108–1114, 1995 (in Chinese). </reference>
		<reference numeration="26" content_type="text"> Yao, T., Qin, D., and Tian, L.: Temperature and precipitation variations on the Tibetan Plateau since 2 ka BP – recorded by Guliya ice core, Sci. China. Ser. D, 26(4), 348–353, 1996 (in Chinese). </reference>
		<reference numeration="27" content_type="text"> Yao, T., Xie, Z., and Wu, Y.: Little Ice Age Climate Record in the Dunde Ice Core, Sci. China. Ser. B, 11, 1196–1201, 1990 (in Chinese). </reference>
		<reference numeration="28" content_type="text"> Yao, T., Xie, Z., Wu, X., and Thompson, L. G.: Climatic change since Little Ice Age recorded by Dunde ice cap, Sci. China Ser. B., 34(6), 760–767, 1991. </reference>
		<reference numeration="29" content_type="text"> Zhang, J., Jin, M., Chen, F., Battarbee, R. W. A., and Henderson, C. G.: Precipitation change on northeastern Tibetan Plateau in the past 800 a recorded in Qinghai lake sediment core, Chinese Sci. B., 49(1), 10–14, 2004 (in Chinese). </reference>
	</references>
</article>

