Received date: 2005-10-19
Revised date: 2006-01-11
Online published: 2006-03-25
Supported by
"Hundred Talent Program" of CAS; National Natural Science Foundation of China, No.40401054; No.40121101; National Basic Research Program of China, No.2005CB422004; Knowledge Innovation Project of the Chinese Academy of Sciences, No.KZCX3-SW-339; President Foundation of CAS
As the "third pole" of the world, the Tibetan Plateau has important effects on climate in its surrounding areas and the whole world. Achievements have been gained on climate change since the last inter-glacial period in recent decades from ice core, tree-ring, and lake sediment records over the Tibetan Plateau. In this paper, we reviewed these achievements, especially those in the special periods. During the last inter-glacial period, temperature dropped rapidly and rose slowly. The temperature record of the last glacial period is consistent with Greenland ice core records, also having its own trait over the Tibetan Plateau. Younger Dryas event agrees with the records from Europe and Greenland. It is warm generally in Holocene, and temperature has been rising in the last 2000 years and gone up rapidly in the last decades. Climate changes at different scales on the Tibetan Plateau occur earlier and the extent is greater than that in other parts of China.
Key words： Tibetan Plateau; climate change; ice core; tree-ring; lake sediment
LI Chaoliu, KANG Shichang . Review of Studies in Climate Change over the Tibetan Plateau[J]. Acta Geographica Sinica, 2006 , 61(3) : 327 -335 . DOI: 10.11821/xb200603012
[1] Wang Shaowu. Introduction to Climate Change. Beijing: China Meteorological Press, 1994. 54-59.
[王绍武. 气候系统引论. 北京: 气象出版社, 1994. 54-59.]
[2] Yao Tandong, Wang Ninglian. The past, present and future of ice core research. Chinese Science Bulletin, 1997, 42(3): 225-230.
[姚檀栋, 王宁练. 冰芯研究的过去、现在和未来. 科学通报, 1997, 42(3): 225-230.]
[3] Alley R B, Meese D A, Shuman C A et al. Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event. Nature, 1993, 362: 527-529.
[4] Yao Tandong. Ice core research and global change. Bulletin of the Chinese Academy of Sciences, 1996, (5): 368-371.
[姚檀栋. 冰芯研究与全球变化. 中国科学院院刊, 1996, (5): 368-371.]
[5] Chen Tuo, Qin Dahe, Li Jiangfeng et al. Response of CO2 concentration parameters and water-use efficiency derived from tree-ring to atmospheric CO2 increase. Journal of Glaciology and Geocryology, 2001, 23(1): 41-45.
[陈拓, 秦大河, 李江风 等. 从树轮纤维素?啄13C 序列看树木生长对大气CO2浓度变化的响应. 冰川冻土, 2001, 23 (1): 41-45.]
[6] Feng Song, Yao Tandong, Jiang Hao. Climate change in recent 600 years over Tibetan Plateau. Plateau Meteorology, 2001, 20(1): 105-108.
[冯松, 姚檀栋, 江灏. 青藏高原近600年的温度变化. 高原气象, 2001, 20(1): 105-108.]
[7] Yao Tandong, L G Thompson, Shi Yafeng et al. Research on climate change since the last inter-glacial period from Guliya ice core. Science in China (D), 1997, 27(5): 447-452.
[姚檀栋, Thompson L G, 施雅风 等. 古里雅冰芯中末次间冰期以来气候变化记录研究. 中国科学(D辑), 1997, 27(5): 447-452.]
[8] Grootes P M, Stuiver M, White J C. Comparison of oxygen isotope records from GISP2 and GRIP Greenland ice cores. Nature, 1993, 366: 552-554.
[9] Wu Jinglu, Wang Sumin. The last inter-glacial climate trait of eastern part of Qinghai-Tibet Plateau recovered from RM hole carbonate oxygen isotope. Chinese Science Bulletin, 1996, 41(11): 1601-1604.
[吴敬禄, 王苏民. 青藏高原东部RM孔碳酸盐氧同位素揭示的末次间冰期气候特征. 科学通报, 1996, 41(11): 1601-1604.]
[10] Xu Xiaobin, Wang Jian, Zhu Jie et al. Study on glacial erosion surface of the southeast of Qinghai-Xizang Plateau using cosmogenic isotopes dating. Scientia Geographica Sinica, 2004, 24(1): 101-104.
[徐孝彬, 王建, 朱捷 等. 利用宇生核素测年技术对青藏高原东南部冰蚀面年代的研究. 地理科学, 2004, 24(1): 101-104.]
[11] Tang Lingyu, Shen Caiming, Kong Zhaochen et al. Pollen evidence of climate during the last glacial maximum in eastern Tibetan Plateau. Journal of Glaciology and Geocryology, 1998, 20(2): 42-49.
[唐领余, 沈才明, 孔昭宸 等. 青藏高原东部末次冰期最盛期气候的花粉证据. 冰川冻土, 1998, 20(2): 42-49.]
[12] Shi Yafeng, Liu Xiaodong, Li Bingyuan. The extremely strong summer monsoon during last 40-30 ka over Tibetan Plateau and its relationship with precessional cycle. Chinese Science Bulletin, 1999, 44(14): 1475-1480.
[施雅风, 刘晓东, 李炳元. 距今40-30 ka青藏高原特强夏季风事件及其与岁差周期关系. 科学通报, 1999, 44(14): 1475-1480.]
[13] Yang Zhihong, Yao Tandong. Younger Dryas event recorded in Guliya ice core. Chinese Science Bulletin, 1997, 42(18): 1975-1978.
[杨志红, 姚檀栋. 古里雅冰芯中的新仙女木期事件记录. 科学通报, 1997, 42(18): 1975-1978.]
[14] Pettet D. Global Younger Dryas. Quaternary International, 1995, 28: 93-104.
[15] Yao Tandong, Yang Zhihong. Qinghai-Tibet Plateau temperature increase showed from ice core records. Chinese Science Bulletin, 1994, 39(5): 438- 441.
[姚檀栋, 杨志红. 冰芯记录所揭示的青藏高原升温. 科学通报, 1994, 39(5): 438- 441.]
[16] Gasse F, Arnold M, Fontes J C et al. A 13,000-year climate record from western Tibet. Nature, 1991, 353: 742-745.
[17] Liu Xingqi, Shen Jie, Wang Sumin et al. Pollen record and the evolution of palaeoclimatology over 16 ka in Qinghai Lake. Chinese Science Bulletin, 2002, 47(17): 1351-1354.
[刘兴起, 沈吉, 王苏民 等. 青海湖16 ka以来的花粉记录及其古气候古环境演化. 科学通报, 2002, 47(17): 1351-1354.]
[18] Lin Zhenyao, Wu Xiangding. Climate division of Qinghai-Tibet Plateau. Acta Geographica Sinica, 1981, 36(1): 22- 32.
[林振耀, 吴祥定. 青藏高原气候区划. 地理学报, 1981, 36(1): 22- 32.]
[19] Broceker W S, Andrge M et al. The chronology of the last deglaciation: implication of Younger Dryas Event. Paleoceanography, 1988, 3(1): 1-19.
[20] Zhu Liping, Wang Junpo, Chen Ling et al. 20,000-year environmental change reflected by multidisciplinary lake sediments in Chen Co, southern Tibet. Acta Geographica Sinica, 2004, 59(4): 514-524.
[朱立平, 王君波, 陈玲 等. 藏南沉错湖泊沉积多指标揭示的2万年以来环境变化. 地理学报, 2004, 59(4): 514-524.]
[21] Smith H J. Ice-sheet-driven shifts. Science, 2000, 289: 1435.
[22] He Yuanqing, Yao Tandong, Shen Yongping. Climatic differences in China during the Holocene indicated by the various climatic proxy data from different parts of China. Journal of Glaciology and Geocryology, 2003, 25(1): 11-18.
[何元庆, 姚檀栋, 沈永平. 冰芯与其它记录所揭示的中国全新世大暖期变化特征. 冰川冻土, 2003, 25(1): 11-18.]
[23] Kutzbach, J E, Guetter P J. Influence of changing orbital parameters and surface boundary conditions on climate simulations for past 18,000 years. Journal of the Atmospheric Sciences, 2002, 43(16): 1726-1759.
[24] Li Yuanfang, Zhang Qingsong, Li Bingyuan. Stracod fauna and environmental changes during the past 17000 years in the western Tibet. Acta Geographica Sinica, 1994, 49(1): 46-54.
[李元芳, 张青松, 李炳元. 青藏高原西北部17000年以来的介形类及环境演变. 地理学报, 1994, 49(1): 46-54.]
[25] Wu Zhonghai, Zhao Xitao, Wu Zhenhan. Geological records of climate and environment changes during the Holocene in the Nam Co Lake and its adjacent areas. Journal of Glaciology and Geocryology, 2004, 26(3): 275-283.
[吴中海, 赵希涛, 吴珍汉. 西藏纳木错及邻区全新世气候与环境变化的地质记录. 冰川冻土, 2004, 26(3): 275-283.]
[26] Hong Bing, Lin Qinghua, Hong Yetang et al. Evolution of southeast monsoon in the eastern part of Qinghai-Tibet during Holocene. Earth and Environment, 2004, 32(1): 42-49.
[洪冰, 林庆华, 洪业汤 等. 全新世青藏高原东部西南季风的演变. 地球与环境, 2004, 32(1): 42-49.]
[27] Liu Guangxiu, Shi Yafeng, Shen Yongping et al. Holoceme Megathermal environment in the Tibetan Plateau. Journal of Glaciology and Geocryology, 1997, 19(2): 114-123.
[刘光秀, 施雅风, 沈永平 等. 青藏高原全新世大暖期环境特征之初步研究. 冰川冻土, 1997, 19(2): 114-123.]
[28] Shi Yafeng, Kong Zhaochen. Climate fluctuation and vital events of Holocene in China. Science in China (B), 1992(12): 1300-1308.
[施雅风, 孔昭宸. 中国全新世大暖期的气候波动与重要事件. 中国科学(B辑), 1992, (12): 1300-1308.]
[29] Yao Tandong, Yang Zhihong, Jiao Keqin et al. A study of climate and environment in the past 2000 years based on ice cores. Earth Science Frontiers, 1997, 4(1-2): 95-100.
[姚檀栋, 杨志红, 焦克勤 等. 近2000年来气候环境变化的冰芯记录研究. 地学前缘, 1997, 4(1-2): 95-100.]
[30] Yao Tandong. Climate change since Little Ice Age from Guliya ice core. Science in China (B), 1995, 25(10): 1108-1114.
[姚檀栋. 古里雅冰芯中小冰期以来的气候变化. 中国科学 (B辑), 1995, 25(10): 1108-1114.]
[31] Kang Xingcheng, Zhang Qihua, Grau mlich L J. Reconstruction and variation of climate in Dulan region, Qinghai during last 2000 years. Advance in Earth Sciences, 2000, 15(2): 215-221.
[康兴成, 张其花, Grau mlich L J. 青海都兰过去2000年来的气候重建及其变迁. 地球科学进展, 2000, 15(2): 215-221.]
[32] Zhang Pengxi, Zhang Baozhen, Qian Guimin et al. Research on palaeoclimatology parameters in Qinghai Lake since Holocene. Quaternary Sciences, 1994, (3): 225-238.
[张彭熹, 张保珍, 钱桂敏 等. 青海湖全新世以来古环境参数的研究. 第四纪研究, 1994, (3): 225-238.]
[33] Yang Bao. Climatic history of Tibetan Plateau during the last 2000 years. Advance in Earth Sciences, 2003, 18(2): 285-291.
[杨保. 青藏高原地区过去2000年来的气候变化. 地球科学进展, 2003, 18(2): 285-291.]
[34] Shao Xuemei, Huang Lei, Liu Hongbin et al. Reconstruction of precipitation variation from tree rings in recent 1000 years in Delingha, Qinghai. Science in China (D), 2004, 34(2): 145-153.
[邵雪梅, 黄磊, 刘洪滨 等. 树轮记录的青海德令哈地区千年降水变化. 中国科学(D辑), 2004, 34(2): 145-153.]
[35] Yao Tandong, Yang Meixue, Kang Xingcheng. Comparative study of the climate changes in the past 2000 years through ice core and the ring records. Quaternary Sciences, 2001, 21(6): 514-519.
[姚檀栋, 杨梅学, 康兴成. 从古里雅冰芯与祁连山树轮记录看过去2000年气候变化. 第四纪研究, 2001, 21(6): 514-519.]
[36] Gong Gaofa, Hameed S. The relationship between temperature and wetness changes during recent 2000 years in China. Beijing: China Meteorological Press, 1993. 70-77.
[龚高法, Hameed S. 近2000年来中国温度变化与湿润状况变化之间的关系. 气候变化及其影响. 北京: 气象出版社, 1993. 70-77.]
[37] Yao Tandong, Duan Keqin, Tian Lide et al. Record of Dasuopu ice core accumulated amount and the variation of Indian monsoon during the last 400 years. Science in China (D), 2000, 30(6): 619-627.
[姚檀栋, 段克勤, 田立德 等. 达索普冰芯积累量记录和过去400年来印度夏季风降水变化. 中国科学(D辑), 2000, 30(6): 619-627.]
[38] Lin Zhenyao. Spacial characteristics of temperature and precipitation changes in Tibetan Plateau. Science in China (D), 1996, 26(4): 254-258.
[林振耀. 青藏高原气温降水变化的空间特征. 中国科学(D辑), 1996, 26(4): 254-258.]
[39] Feng Song, Tang Baocang, Wang Dongmei. New evidence supporting Tibetan Plateau as the trigger region of China. Chinese Science Bulletin, 1998, 43(6): 633-636.
[冯松, 汤懋苍, 王冬梅. 青藏高原是我国气候变化启动区的新证据. 科学通报, 1998, 43(6): 633-636.]
[40] Liu Xiaodong, Hou Ping. Relationship between climatic warming over Qinghai-Tibet Plateau and its surrounding areas in recent 30 years and the elevation. Plateau Meteorology, 1998, 17: 245-249.
[刘晓东, 侯萍. 青藏高原及邻近地区近30年气候变暖与海拔高度的关系. 高原气象, 1998, 17: 245-249.]
[41] Yao Tandong, Liu Xiaodong. The climate change extent of the Qinghai-Tibet Plateau. Chinese Science Bulletin, 2000, 45(1): 98-106.
[姚檀栋, 刘晓东. 青藏高原地区的气候变化幅度问题. 科学通报, 2000, 45(1): 98-106.]
[42] Yang Bao, Kang Xingcheng, Shi Yafeng. Decadal climatic variations indicated by Dulan tree-ring and the comparison with temperature proxy data from other regions of China during the last 2000 years. Scientia Geographica Sinica, 2000, 20(5): 397-402.
[杨保, 康兴成, 施雅风. 近2000年都兰树轮10 年尺度的气候变化及其与中国其它地区温度代用资料的比较. 地理科学, 2000, 20(5): 397-402.]
[43] Stocker T F, Schmittner A. Influence of CO2 emission rates on the stability of the thermohaline circulation. Nature, 1997, 388: 862-865.
[44] Liu Xiaodong, Ma Zhuguo. An important cause leading to short-term climatic variation in China: the change in the surface albedo in Tibetan Plateau. Journal of Tropical Meteorology, 1996, 12(3): 240-245.
[刘晓东, 马柱国. 中国短期气候变化的一个重要原因: 青藏高原地表反射率的变化. 热带气象学报, 1996, 12(3): 240-245.]
[45] Lin Zhenyao, Wu Xiangding. Tibetan Climate. Beijing: Science Press, 1984. 145.
[林振耀, 吴祥定. 西藏气候. 北京: 科学出版社, 1984. 145.]
[46] Bond G, Kumer B, Beer J et al. Persistent so1ar influence on North Atlantic climate during the Holocene. Science, 2001, 294: 2130-2136.
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