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Twentieth-century warming preserved in a Geladaindong mountain ice core, central Tibetan Plateau

Published online by Cambridge University Press:  03 March 2016

Yulan Zhang ,
Shichang Kang ,
Bjorn Grigholm ,
Yongjun Zhang ,
Susan Kaspari ,
Uwe Morgenstern ,
Jiawen Ren ,
Dahe Qin ,
Paul A. Mayewski  and
Qianggong Zhang
...Show all authors
Yulan Zhang
Affiliation:
State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, China Laboratory of Green Chemistry, Lappeenranta University of Technology, Mikkeli, Finland
Shichang Kang*
Affiliation:
State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, China CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing, China
Bjorn Grigholm
Affiliation:
Climate Change Institute and Department of Earth Sciences, University of Maine, Orono, ME, USA
Yongjun Zhang
Affiliation:
Key Laboratory of Tibetan Environment Changes and Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Susan Kaspari
Affiliation:
Department of Geological Sciences, Central Washington University, Ellensburg, WA, USA
Uwe Morgenstern
Affiliation:
Institute of Geological and Nuclear Sciences, National Isotope Centre, Lower Hutt, New Zealand
Jiawen Ren
Affiliation:
State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, China
Dahe Qin
Affiliation:
State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, China
Paul A. Mayewski
Affiliation:
Climate Change Institute and Department of Earth Sciences, University of Maine, Orono, ME, USA
Qianggong Zhang
Affiliation:
CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing, China Key Laboratory of Tibetan Environment Changes and Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Zhiyuan Cong
Affiliation:
CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing, China Key Laboratory of Tibetan Environment Changes and Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Mika Sillanpää
Affiliation:
Laboratory of Green Chemistry, Lappeenranta University of Technology, Mikkeli, Finland
Margit Schwikowski
Affiliation:
Laboratory of Radiochemistry and Environmental Chemistry, Paul Scherrer Institut, Villigen PSI, Switzerland
Feng Chen
Affiliation:
Key Laboratory of Tibetan Environment Changes and Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
*
Correspondence: Shichang Kang <shichang.kang@lzb.ac.cn>
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Abstract

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High-resolution δ18O records from a Geladaindong mountain ice core spanning the period 1477-1982 were used to investigate past temperature variations in the Yangtze River source region of the central Tibetan Plateau (TP). Annual ice-core δ18O records were positively correlated with temperature data from nearby meteorological stations, suggesting that the δ18O record represented the air temperature in the region. A generally increasing temperature trend over the past 500 years was identified, with amplified warming during the 20th century. A colder stage, spanning before the 1850s, was found to represent the Little Ice Age with colder periods occurring during the 1470s–1500s, 1580s–1660s, 1700s–20s and 1770s–1840s. Compared with other temperature records from the TP and the Northern Hemisphere, the Geladaindong ice-core record suggested that the regional climate of the central TP experienced a stronger warming trend during the 20th century than other regions. In addition, a positive relationship between the Geladaindong δ18 O values and the North Atlantic Oscillation index, combined with a wavelet analysis of δ18 O records, indicated that there was a potential atmospheric teleconnection between the North Atlantic and the central TP.

Keywords

climate changeice chronology/datingice core
Type
Paper
Information
Annals of Glaciology , Volume 57 , Issue 71 , March 2016 , pp. 70 - 80
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.
Copyright
Copyright © The Author(s) 2016

References

Allan, R and Ansell, T (2006) A new globally-complete monthly historical gridded mean sea level pressure data set (HadSLP2): 1850-2004. J. Climatol., 19(22), 5816–5842 (doi: 10.1175/jcli3937.1)Google Scholar
Beck, HL and Bennett, BC (2002) Historical overview of atmospheric nuclear weapons testing and estimates of fallout in the continental United States. Health Phys., 82(5), 591–608 (doi: 10.1097/00004032-200205000-00007)Google Scholar
Bräuning, A (2006) Tree-ring evidence of ‘Little Ice Age’ glacier advances in southern Tibet. Holocene, 6(3), 369–380 (doi: 10.1191/0959683606h1 922rp)Google Scholar
Davis, ME, Thompson, LC, Yao, T and Wang, N (2005) 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)Google Scholar
Eichler, A and 7 others (2000) Claciochemical dating of an ice core from upper Crenzgletscher (4200ma.s.l.). J. Glaciol., 46(154), 507–515 (doi: 10.3189/172756500781833098)Google Scholar
Eichler, A, Schwikowski, M and Gäggeler, H (2001) Meltwater-induced relocation of chemical species in Alpine firn. Tellus B, 53(2), 192–203 (doi: 10.1034/j.1600-0889.2001.d01-15.x)Google Scholar
Fujita, K, Ageta, Y, Pu, J and Yao, T (2000) Mass balance of Xiao Dongkemadi glacier on the central Tibetan Plateau from 1989 to 1995. Ann. Glaciol., 31, 159–163 (doi: 10.3189/172756400781820075. 2000)Google Scholar
Gäggeler, HW, von Cunten, HR, Oeschger, H and Schotterer, U (1983) 210Pb-dating of cold alpine firn/ice cores from Colle Gnifetti, Switzerland. J. Glaciol., 29(101), 165–177 Google Scholar
Gou, X, Chen, F, Yang, M, Jacoby, C, Peng, J and Zhang, Y (2006) A comparison of tree-ring records and glacier variations over the past 700 years, northeastern Tibetan Plateau. Ann. Glaciol., 43, 86–90 (doi: 10.3189/172756406781812438)CrossRefGoogle Scholar
Grigholm, B and 6 others (2009) Atmospheric soluble dust from a Tibetan ice core: possible climate proxies and teleconnection with the Pacific Decadal Oscillation. J. Geophys. Res., 114, D20118 (doi: 10.1029/2008JD011242)Google Scholar
Hurrell, JW, Kushnir, Y and Visbeck, M (2001) The North Atlantic Oscillation. Science, 291, 603–604 (doi: 10.1126/science.1058761)Google Scholar
Hurrell, JW, Kushnir, Y, Ottersen, G and Visbeck, M (2003) An overview of the North Atlantic Oscillation. In Hurrell, JW, Kushnir, Y, Ottersen, C and Visbeck, M eds The North Atlantic Oscillation: climatic significance and environmental impact.(Geophysical Monograph Series, 134) American Geophysical Union, Washington, DC, 1–35 CrossRefGoogle Scholar
Immerzeel, WW, Van Beek, LPH and Bierkens, MEP (2010) Climate change will affect the Asian water tower. Science, 328, 1382–1385 (doi: 10.1126/science.1183188)Google Scholar
Jones, PD, Jonsson, T and Wheeler, D (1997) Extension to the North Atlantic Oscillation using early instrumental pressure observations from Gibraltar and south-west Iceland. J. Climatol, 17(13), 1433–1450 (doi: 10.1002/(sici)1097-0088(19971115) 17:13<1433::aid-joc203>3.0.co;2-p)Google Scholar
Jones, PD, Osborn, TJ and Briffa, KR (2003) Pressure-based measures of the North Atlantic Oscillation (NAO): a comparison and an assessment of changes in the strength of the NAO and its influence on surface climate parameters. In Hurrell, JW, Kushnir, Y, Ottersen, G and Visbeck, M eds The North Atlantic Oscillation: climatic significance and environmental impact.(Geophysical Monograph Series, 134) American Geophysical Union, Washington, DC, 51–62 (doi: 10.1029/1 34GM03)CrossRefGoogle Scholar
Joswiak, DR, Yao, T, Wu, G, Xu, B and Zheng, W (2010) A 70-a record of oxygen-18 variability in an ice core from the Tanggula Mountains, central Tibetan Plateau. Climate Past, 6, 219–227 Google Scholar
Jouzel, J and 6 others (2003) Magnitude of isotope/temperature scaling for interpretation of central Antarctic ice cores. J. Geophys. Res., 108(D12) (doi: 10.1029/2002JD002677)Google Scholar
Kang, S and 6 others (2007) Recent temperature increase recorded in an ice core in the source region of Yangtze River. Chinese Sci. Bull., 52(6), 825–831 (doi: 10.1007/s11434-007-0140-1)CrossRefGoogle Scholar
Kang, S and 7 others (2010) Variability of atmospheric dust loading over the central Tibetan Plateau based on ice core glaciochemistry. Atmos. Environ., 44, 2980–2989 (doi: 10.1016/j.atmosenv. 2010.05.014)Google Scholar
Kang, S and 10 others (2015) Dramatic loss of glacier accumulation area on the Tibetan Plateau revealed by ice core tritium and mercury records. Cryosphere, 9, 1–10 (doi: 10.5194/tc-9-1-2015)Google Scholar
Kaspari, S, Hooke, RLeB, Mayewski, PA, Kang, SC, Hou, SG and Qin, DH (2008) Snow accumulation rate on Qomolangma (Mount Everest), Himalaya: synchroneity with sites across the Tibetan Plateau on 50-100 year timescales. J. Glaciol., 54(185), 343–352 (doi: 10.3189/002214308784886126)Google Scholar
Kaspari, S and 7 others (2009) Recent increases in atmospheric concentrations of Bi, U, Cs, S and Ca from a 350-year Mount Everest ice core record. J. Geophys. Res., 114, D04302 (doi: 10.1029/2008JD011088)Google Scholar
Kehrwald, NM and 8 others (2008) Mass loss on Himalayan glacier endangers water resources. Geophys. Res. Lett, 35, L225O3 (doi: 10.1029/2008GL035556)Google Scholar
Li, J and 6 others (1986) Glaciers in Tibet. Science Press, Beijing Google Scholar
Liang, E, Shao, X and Liu, X (2009) Annual precipitation variation inferred from tree rings since A.D. 1 770 for the western Qilian Mts., northern Tibetan Plateau. Tree-Ring Res., 65(2), 95–103 (doi: 10.3959/2008-2.1)Google Scholar
Liu, X and Yin, Z (2001) Spatial and temporal variation of summer precipitation over the eastern Tibetan Plateau and the North Atlantic oscillation. J. Climate, 14, 2896–2909 (doi: 10.1175/1520-0442(2001)014<2896:satvos>2.0.co;2)Google Scholar
Morgenstern, U and Taylor, CB (2009) Ultra low-level tritium measurement using electrolytic enrichment and LSC. Isot. Environ. Health Stud., 45(2), 96–117 (doi: 10.1080/10256010902931194)Google Scholar
Nakazawa, F and Fujita, K (2006) Use of ice cores from glaciers with melting for reconstructing mean summer temperature variations. Ann. Glaciol., 43, 167–171 (doi: 10.3189/172756406781812302)Google Scholar
Nye, J (1963) Correction factor for accumulation measured by the thickness of the annual layers in an ice sheet. J. Glaciol., 4(36), 785–788 CrossRefGoogle Scholar
Pu, J and 6 others (2008) Rapid decrease of mass balance observed in the Xiao (Lesser) Dongkemadi Glacier, in the central Tibetan Plateau. Hydrol. Process., 22(16), 2953–2958 (doi: 10.1002/hyp.6865)Google Scholar
Radić, V and Hock, R (2011) Regionally differentiated contribution of mountain glaciers and ice caps to future sea-level rise. Nature Geosci., 4(2), 91–94 (doi: 10.1038/NGEO1052)Google Scholar
Shi, Y (2008) Concise glacier inventory of China. Shanghai Popular Science Press, Shanghai Google Scholar
Stocker, TF and 9 others eds (2013) Climate change 2013: the physical science basis. Contribution of Working Group 1 to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge and New York Google Scholar
Thompson, DWJ and Wallace, JM (2001) Regional climate impacts of the Northern Hemisphere annular mode. Science, 293(5527), 85–89 (doi: 10.1126/science.1058958)CrossRefGoogle ScholarPubMed
Thompson, LG, Yao, T, Mosley-Thompson, E, Davis, ME, Henderson, KA and Lin, P-N (2000) A high-resolution millennial record of the south Asian monsoon from Himalayan ice core. Science, 289(5486), 1916–1919 (doi: 10.1126/science.289. 5486.1916)Google Scholar
Thompson, LG and 6 others (2006a) Ice core evidence for asynchronous glaciation on the Tibetan Plateau. Quat. Int., 154–155, 3-10 (doi: 10.101 6/j.quaint.2006.02.001)Google Scholar
Thompson, LG and 7 others (2006b) Holocene climate variability archived in the Puruogangri ice cap on the central Tibetan Plateau. Ann. Glaciol., 43, 61–67 (doi: 10.3189/172756406781812357)Google Scholar
Tian, L, Yao, T, Sun, W, Stievenard, W and Jouzel, J (2001a) Relationship between delta D and delta O-18 in precipitation on north and south of the Tibetan Plateau and moisture recycling. Sci J. China, Ser. D, 44(9), 789–796 (doi: 10.1007/BfO29O7O91)Google Scholar
Tian, L, Masson-Delmotte, V, Stievenard, M, Yao, T and Jouzel, J (2001b) Tibetan Plateau summer monsoon northward extent revealed by measurements of water stable isotopes. J. Geophys. Res., 106(D22), 28 081–28 088 (doi: 10.1029/2001JD9001 86)Google Scholar
Tian, L and 7 others (2007) Stable isotopic variations in west China: a consideration of moisture sources. J. Geophys. Res., 112, D10112 (doi: 10.1029/2006JD007718)Google Scholar
Wang, N, Thompson, LC, Davis, ME and Mosley-Thompson, E (2003) Influence of variations in NAO and SO on air temperature over the northern Tibetan Plateau as recorded by δ18O in the Malan ice core. Geophys. Res. Lett, 30, 222167 (doi: 10.1029/2003CL018188)Google Scholar
Wang, S, Wen, X, Luo, Y, Dong, W, Zhao, C and Yang, B (2007) Reconstruction of temperature series of China for last 1000 years. Chinese Sci. Bull., 52(23), 3272–3280 (doi: 10.1007/s11434-007-0425-4)Google Scholar
Xu, J and 6 others (2007) Dust storm activity over the Tibetan Plateau recorded by a shallow ice core from the north slope of Mt. Qomolangma (Everest), Tibet-Himalayan region. Geophys. Res. Lett, 34, L17504 (doi: 10.1029/2007CL030853)Google Scholar
Xu, J, Kaspari, S, Hou, S, Kang, S, Qin, D, Ren, J and Mayewski, PA (2009) Records of volcanic events since AD 1800 in the East Rongbuk ice core from Mt. Qomolangma. Chinese Sci. Bull., 54(8), 1411–1416 (doi: 10.1007/s11434-009-0020-y)Google Scholar
Xu, P, Zhu, H, Shao, X and Yin, Z (2012) Tree ring-dated fluctuation history of Midui glacier since the Little Ice Age in the southeastern Tibetan Plateau. Sci. China (Earth Sci.), 55(4), 521–529 (doi: 10.1007/s11430-011-4338-3)Google Scholar
Xu, X and Yi, C (2014) Little Ice Age on the Tibetan Plateau and its bordering mountains: evidence from moraine chronologies. Global Planet. Change, 116, 41–53 (doi: 10.1016/j.glopla-cha.2014.02.003)CrossRefGoogle Scholar
Yanai, M and Wu, C (2005) Effects of the Tibetan Plateau. In Wang, B ed. The Asian Monsoon. Springer, Berlin, 513–549 Google Scholar
Yang, B, Bräuning, A, Dong, Z, Zhang, Z and Jiao, K (2008) Late Holocene monsoonal temperature glacier fluctuations on the Tibetan Plateau. Global Planet. Change, 60, 126–140 (doi: 10.1016/j.gloplacha.2006.07.035)Google Scholar
Yang, B, Bräuning, A, Liu, J, Davis, ME and Shao, Y (2009) Temperature changes on the Tibetan Plateau during the past 600 years inferred from ice cores and tree rings. Global Planet. Change, 69, 71–78 (doi: 10.101 6/j.gloplacha.2009.07.008)Google Scholar
Yang, B, Kang, X, Liu, J, Bräuning, A and Qin, C (2010) Annual temperature history in Southwest Tibet during the last 400 years recorded by tree rings. Int. J. Climatol., 30, 962–971 (doi: 10.1002/joc.1956)Google Scholar
Yao, T, Shi, Y and Thompson, LC (1997) High resolution records of paleoclimate since the Little Ice Age from the Tibetan Plateau. Quat. Int., 37, 19–23 (doi: 10.1016/1040-6182(96)00006-7)Google Scholar
Yao, T and 8 others (2006) δ18O record and temperature change over the past 100 years in ice cores on the Tibetan Plateau. Sci .China, 49(1), 1–9 (doi: 10.1007/s11430-004-5096-2)Google Scholar
Yao, T and 7 others (2007) Temperature variations over the past millennium on the Tibetan Plateau revealed by four ice cores. Ann. Glacioi, 46, 362–366 (doi: 10.3189/172756407782871305)Google Scholar
Yao, T and 14 others (2012) Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings. Nature Climate Change (doi: 10.1038/NCLMATE1580)Google Scholar
Yao, T and 13 others (2013) A review of climatic controls on δ18O in precipitation over the Tibetan Plateau: observations and simulations. Rev. Geophys., 51, 1–24 (doi: 8755-1209/13/10.1002/rog.20023)Google Scholar
Ye, Q, Kang, S, Chen, F and Wang, J (2006) Monitoring glacier variations on Celadandong mountain, central Tibetan Plateau, from 1969 to 2002 using remote-sensing and GIS technologies. J. Glacioi, 52(179), 537–545 (doi: 10.3189/172756506781828359)Google Scholar
You, Q and 6 others (2010) Climate warming and associated changes in atmospheric circulation in the eastern and central Tibetan Plateau from a homogenized dataset. Global Planet. Change, 72, 11–24 (doi: 10.1016/j.gloplacha.2010.04.003)Google Scholar
Yu, R and Zhou, T (2004) Impacts of winter-NAO on March cooling trends over subtropical Eurasia continent in the recent half century. Geophys. Res. Lett, 31, L12204 (doi: 10.1029/2004CL019814)Google Scholar
Zhang, G, Li, Z, Wang, W and Wang, W (2014) Rapid decrease of observed mass balance in the Urumqi Glacier No.1, Tianshan Mountains, central Asia. Quat. Int., 349, 135–141 (doi: 10.101 6/j.quaint.2O1 3.08.035)Google Scholar
Zhang, Y, Kang, S, Zhang, Q, Cong, Z and Zhang, Y (2007) Snow ice records on Mt. Geladaindong in the central Tibetan Plateau. J.Glacioi. Geocryol., 29(5), 685–693 [in Chinese with English summary]Google Scholar
Zhao, H and 6 others (2011) Deuterium excess record in a southern Tibetan ice core and its potential climatic implications. Climate Dyn., 38(9-10), 1791–1803 (doi: 10.1007/s00382-011-1161-7)Google Scholar
Zhu, H, Xu, P, Shao, X and Luo, H (2012) Little Ice Age glacier fluctuations reconstructed for the southeastern Tibetan Plateau using tree rings. Quat. Int., 283, 134–138 (doi: 10.1016/j.quaint.2012.04.011)Google Scholar