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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>6</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/cp-6-475-2010</doi>
	<article_url>http://www.clim-past.net/6/475/2010/</article_url>
	<abstract_html>http://www.clim-past.net/6/475/2010/cp-6-475-2010.html</abstract_html>
	<fulltext_pdf>http://www.clim-past.net/6/475/2010/cp-6-475-2010.pdf</fulltext_pdf>
	<start_page>475</start_page>
	<end_page>481</end_page>
	<publication_date>2010-07-26</publication_date>
	<article_title content_type="html">Characteristics of cold–warm variation in the Hetao region and its surrounding areas in China during the past 5000 years</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>M.-Q. Li</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>Q.-S. Ge</name>
			<email>geqs@igsnrr.ac.cn</email>
		</author>
		<author numeration="3" affiliations="1">
			<name>Z.-X. Hao</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>J.-Y. Zheng</name>
		</author>
		<author numeration="5" affiliations="1,2">
			<name>S.-F. He</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China</affiliation>
		<affiliation numeration="2" content_type="html">Graduate School of the Chinese Academy of Sciences, Beijing 100049, China</affiliation>
	</affiliations>
	<abstract content_type="html">Using six long-term temperature proxy data series derived from different
natural evidences, including pollens and lake-sediments, we reconstructed a
temperature series with a 100-yr time resolution for the past 5000 yr in the
Hetao region and its surrounding areas. The resulting series suggests that,
on a millennial timescale, temperatures in the region were higher than the
mean value of the whole series during the 5000~2600 years before
present (yr BP) period, and became relatively low comparing with the average
temperature of the whole series after 2600 yr BP. Within these two periods,
temperature fluctuations comprising numerous short, multi-centennial
intervals also existed. A comparison between our reconstructed series and
other series in China and across the Northern Hemisphere indicate that, on a
long-term scale, cold–warm variations had been in phase across the whole
hemisphere during the past 5000 years; on the century to multi-century
scale, the beginning and the ending times varied from region to region, thus
implying that climate changes did not occur simultaneously in different
regions.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Axford, Y., Miller, G. H., Geirsd&apos; ottir, A&apos;., et al.: Holocene temperature history of Northern Iceland inferred from subfossil midges, Quaternary Sci. Rev., 26, 3344–3358, 2007. </reference>
		<reference numeration="2" content_type="text"> Bianchi, G. G. and Mccave, I. N.: Holocene periodicity in North Atlantic climate and deep-ocean flow, south of Iceland, Nature, 397, 515–516, 1999. </reference>
		<reference numeration="3" content_type="text"> Bond, G. C. and Showers, W.: A pervasive millennial-scale cycle in the North Atlantic Holocene and glacial climate, Science, 278, 1257–1265, 1997. </reference>
		<reference numeration="4" content_type="text"> Bond, G., Kromer, B., Beer, J., et al.: Persistent solar influence on North Atlantic climate during the Holocene, Science, 294, 2130–2136, 2001. </reference>
		<reference numeration="5" content_type="text"> Bradley, R. S. and Jones, P. D.: &quot;Little ice age&quot; summer temperature variations: their nature and relevance to recent global warming trends, The Holocene, 3, 367–376, 1993. </reference>
		<reference numeration="6" content_type="text"> Chen, C.-T. A., Lan, H.-C., Lou, J.-Y., et al.: The dry Holocene megathermal in Inner Mongolia, Palaeogeogr. Palaeocl., 193, 181–200, 2003. </reference>
		<reference numeration="7" content_type="text"> Chu, K. C.: A preliminary study on the climatic fluctuation during the last 5000 years in China, Sci. Sinica, XVI, 226–256, 1973. </reference>
		<reference numeration="8" content_type="text"> Cronin, T. M., Dwyer, G. S., Kamiya, T., et al.: Medieval warm period, little ice age and 20th century temperature variability from Chesapeake Bay, Global Planet. Change, 36, 17–29, 2003. </reference>
		<reference numeration="9" content_type="text"> Crowley, T. J. and Lowery, T. S.: How warm was the MedievalWarm Period?, Ambio, 29, 51–54, 2000. </reference>
		<reference numeration="10" content_type="text"> Cui, M. L., Luo, Y. L., and Sun, X. J.: Paleovegetational and paleoclimatic changes in Ha&apos;ni Lake, Jilin since 5 ka BP, Mar. Geol. Quat. Geol., 26, 117–122, 2006. </reference>
		<reference numeration="11" content_type="text"> Ge, Q. S., Wang, S. B., and Zheng, J. Y.: Reconstruction of temperature series in China for the last 5000 yr, Prog. Nat. Sci., 16, 838–845, 2006. </reference>
		<reference numeration="12" content_type="text"> Ge, Q. S., Zheng, J. Y., Fang, X. Q., et al.: Temperature changes of winter-half-year in Eastern China during the past 2000 yr, The Holocene, 22, 933–940, 2003. </reference>
		<reference numeration="13" content_type="text"> Ge, Q.-S., Zheng, J.-Y., Hao, Z.-X., et al.: temperature variation through 2000 years in China: An Uncertainty Analysis of Reconstruction and regional difference, Geophys. Res. Lett., 37, L03703, doi:10.1029/2009GL041281, 2010. </reference>
		<reference numeration="14" content_type="text"> Hao, Z. X., Ge, Q. S., and Zheng, J. Y.: Temperature variations during the song and Yuan Dynasties (960$\sim $1368 AD) in the eastern part of North West China. Quat. Sci., 29, 871–879, 2009. </reference>
		<reference numeration="15" content_type="text"> Hong, Y. T., Hong, B., Lin, Q. H., et al.: Grain size of quartz as an indicator of winter monsoon strength on the Loess Plateau of central China during Holocene, Earth Planet. Sci. Lett., 211, 371–380, 2003. </reference>
		<reference numeration="16" content_type="text"> Jia, T. F., Yin, S., He, Y., et al.: Holocene sediment texture and its environment meaning of Donghaizi Lake in Ulan Buh Desert, J. Desert Res., 23, 165–170, 2003. </reference>
		<reference numeration="17" content_type="text"> Jin, G. Y. and Liu, T. S.: Mid-Holocene climate change in North China, and the effect on cultural development, Chinese Sci. Bull., 47, 408–413, 2002. </reference>
		<reference numeration="18" content_type="text"> Jin, H. L., Su, Z. Z., Sun, L. Y., et al.: Holocene climatic change in Hunshandake Desert, Chinese Sci. Bull., 49, 1730–1735, 2004. </reference>
		<reference numeration="19" content_type="text"> Jin, Z. D., Shen, J., Wang, S. M., et al.: The medieval warm period in the Daihai area, J. Lake Sci., 14, 209–216, 2002. </reference>
		<reference numeration="20" content_type="text"> Jones, P. D., Briffa, K. R., Barnett, T. P., et al.: High resolution palaeoclimatic records from the last millennium: interpretation, integration and comparison with general circulation model control-run temperatures, The Holocene, 8, 445–471, 1998. </reference>
		<reference numeration="21" content_type="text"> Jones, P. D., Osborn, T. J., and Briffa, K. R.: Estimating sampling errors in larger-scale temperature averages, J. Climatol., 10, 2548–2568, 1999. </reference>
		<reference numeration="22" content_type="text"> Liu, X. H., Shao, X. M., Zhao, L. J., et al.: Dendroclimatic temperature record derived from tree- ring width and stable carbon isotope chronologies in the Middle Qianlian Mountains, China. Arct. Antarct. Alp. Res., 39, 651-657, 2007. </reference>
		<reference numeration="23" content_type="text"> Long, H., Wang, N. A., Li, Y., et al.: Mid-Holocene climate variations from lake records of the east Asian monsoon margin: a multi-proxy and geomorphological study, Quat. Sci., 27, 371–381, 2007. </reference>
		<reference numeration="24" content_type="text"> Lu, H. Y.: Grassland culture and climate change in Northern temperature area since Neolithic Age, Cult. Relic Prot. Archaeol., 3, 44–50, 1991. </reference>
		<reference numeration="25" content_type="text"> Luo, J. Y. and Chen, C. T. A.: Paleoclimatological and paleoenvironmental records since 4000 a BP in sediments of alpine lakes in Taiwan, Sci. China Ser. D, 40, 424–431, 1997. </reference>
		<reference numeration="26" content_type="text"> Mann, M. E. and Jones, P. D.: Global surface temperatures over the past two millennia, Geophys. Res. Lett., 30, 1820–1823, 2003. </reference>
		<reference numeration="27" content_type="text"> Mann, M. E., Bradley, R. S., and Hughes, M. K.: Global-scale temperature patterns and climate forcing over the past six centuries, Nature, 392, 779–787, 1998. </reference>
		<reference numeration="28" content_type="text"> Mann, M. E., Bradley, R. S., and Hughes, M. K.: Northern Hemisphere temperatures during the last millennium: Inferences, uncertainties and limitations. Geophys. Res. Lett., 26, 759–762, 1999. </reference>
		<reference numeration="29" content_type="text"> Mann, M. E., Zhang, Z. H., Hughes, M. K., et al.: Proxy-based reconstructions of hemispheric and global surface temperature variations over the past two millennia, Proc. Natl. Acad. Sci. USA, 105, 13252–13257, 2008. </reference>
		<reference numeration="30" content_type="text"> Moberg, A., Sonechkin, D. M., Holmgren, K., et al.: Highly variable Northern Hemisphere temperatures reconstructed from low- and high-resolution proxy data, Nature, 433, 613–617, 2005. </reference>
		<reference numeration="31" content_type="text"> Peng, H. X., Shi, C. Y., Wei, Y., et al.: Organic carbon stable isotope records of climate evolution in Poyang Lake in the past 5 ka years, J. Cent. China Normal Univ. Nat. Sci., 37, 123–125, 2003. </reference>
		<reference numeration="32" content_type="text"> Qian, Z. H., Kenneth, J. H., and Yuan, Z.: Kataglacial age of quaternary period and climatic characteristics of Holocene epoch – a record of carbon isotope from Yanhaizi Ya02 borehole in Yileague of Inner Mongolia, Geol. Chem. Mineral., 24, 96–101, 2002. </reference>
		<reference numeration="33" content_type="text"> Sepp\&quot; a, H. and Birks, H. J. B.: Holocene climate reconstruction from the Fennoscandian treeline area based on pollen data from Toskaljavri, Quaternary Res., 57, 191–199, 2002. </reference>
		<reference numeration="34" content_type="text"> Shao, X. H., Wang, Y. J., Cheng, H., et al.: Long-term trend and abrupt events of the Holocene Asian monsoon inferred from a stalagmite $\delta $18O record from Shennongjia in Central China, Chinese Sci. Bull., 51, 221–228, 2006. </reference>
		<reference numeration="35" content_type="text"> Shen, H. Y., Jia, Y. L., Li, X. S., et al.: Environmental change inferred from distribution of Rb and Sr in different grain size fractions from lacustrine sediments in Huangqihai Lake, Inner Mongolia, Acta Geogr. Sin., 61, 1208–1217, 2006. </reference>
		<reference numeration="36" content_type="text"> Shen, J., Matsumoto, R., Wang, S. M., et al.: Quantitative reconstruction of the lake water paleotemperature of Daihai Lake, Inner Mongolia, China and its significance in paleoclimate, Sci. China Ser. D, 45, 792–800, 2002. </reference>
		<reference numeration="37" content_type="text"> Shi, P. J. and Song, C. Q.: Palynological records of environmental changes in the middle part of Inner Mongolia, China, Chinese Sci. Bull., 48, 1433–1438, 2003. </reference>
		<reference numeration="38" content_type="text"> Stuiver, M., Reimer, B., and Braziunas, T.: High-precision radiocarbon age calibration for terrestrial and marine samples, Radiocarbon, 49, 1127–1151, 1998. </reference>
		<reference numeration="39" content_type="text"> Wang, S. W. and Gong, D. Y.: Enhancement of the warming trend in China, Geophys. Res. Lett., 27, 2581–2584, 2000. </reference>
		<reference numeration="40" content_type="text"> Wang, S. W., Wen, X. Y., Luo, Y., et al.: Reconstruction of temperature series of China for the last 1000 yr, Chinese Sci. Bull., 52, 3272–3280, 2007. </reference>
		<reference numeration="41" content_type="text"> Wang, S. W., Ye, J. L., and Gong, D. Y.: Climate in China during the little ice age, Quat. Sci., 1, 54–64, 1998. </reference>
		<reference numeration="42" content_type="text"> Wang, X. L. and He, Y.: Climate change from 7000 a BP in Xishan Mountain of Zhengzhou by analysis of magnetic susceptibility, J. Beijing Norm. Univ. Nat. Sci., 40, 133–136, 2004. </reference>
		<reference numeration="43" content_type="text"> Xiao, J. L., Nakamura, T., Lu, H. Y., et al.: Holocene climate changes over the desert/loess transition of north-central China, Earth Planet. Sci. Lett., 197, 11–18, 2002. </reference>
		<reference numeration="44" content_type="text"> Xiao, J. L., Xu, Q. H., Nakamura, T., et al.: Holocene vegetation variation in the Daihai Lake region of north-central China: a direct indication of the Asian monsoon climatic history, Quaternary Sci. Rev., 23, 1669–1679, 2004. </reference>
		<reference numeration="45" content_type="text"> Xu, Q. H., Xiao, J. L., Nakamura, T., et al.: Quantitative reconstructed climatic changes of Daihai Basin by pollen data, Marine Geol. Quat. Geol., 23, 99–108, 2003. </reference>
		<reference numeration="46" content_type="text"> Yang, B.: Climate history of the Tibetan Plateau during the last two millennia, Adv. Earth Sci., 18, 285–291, 2003. </reference>
		<reference numeration="47" content_type="text"> Yang, B., Braeuning, A., and Johnson, K. R.: General characteristics of temperature variation in China during the last two millennia, Geophys. Res. Lett., 29, 381–384, 2002. </reference>
		<reference numeration="48" content_type="text"> Yang, B., Braeuning, A., and Shi, Y. F.: Late Holocene temperature fluctuations on the Tibetan Plateau, Quaternary Sci. Rev., 22, 2335–2344, 2003. </reference>
		<reference numeration="49" content_type="text"> Yao, T. D. and Thompson, L. G.: Dunde ice core records and temperature variation in the past 5 ka, Sci. China Ser. B, 10, 1089–1093, 1992. </reference>
		<reference numeration="50" content_type="text"> Yao, T. D., Thompson, L. G., Qin, D. H., et al.: Variations in temperature and precipitation in the past 2000 a on the Xizang (Tibet) Plateau – Guliya ice core record, Sci. China Ser. D, 39, 425–433, 1996. </reference>
		<reference numeration="51" content_type="text"> Yao, T. D., Yang, M. X., and Kang, X. C.: Comparative study of the climate change in the past 2000 yr by using ice core and tree ring records, Quat. Sci., 21, 514–519, 2001. </reference>
		<reference numeration="52" content_type="text"> Zhang, L. S., Fang, X. Q., Ren, G. Y., et al.: Environmental change in the north China farming grazing transitional zone, Earth Sci. Front., 4, 127–136, 1997. </reference>
	</references>
</article>

