Changes of Some Monsoonal Temperate Glaciers in Hengduan Mountains Region during 1900-2007
Received date: 2009-01-24
Revised date: 2009-04-24
Online published: 2009-11-25
Supported by
This study was supported a Major Directionality Program of China's Academy of Sciences (KZCXZ-YW-317), a Project for Incubation of Specialists in Glaciology and Geocryology of National Natural Science Foundation of China (J0630966), a National Basic Research Program of China (2007CB411201), a Key Project of the National Natural Science Foundation of China (90511007), a West Light Foundation of China's Academy of Sciences (O828A11001), a Project of the National Natural Science Foundation of China (40971019, 40801028), and the Foundation from The State Key Laboratory of Cryosphere Science and Lijiang City Government
Since the early 1900s, a tendency for some monsoonal temperate glaciers retreat has been observed in the Hengduan Mountains region. Against the background of climate change, 7 monsoonal temperate glaciers were in a stationary or an advancing state between the 1900s-1930s and the 1960s-1980s, and they were in a retreat state during the 1930s-1960s and from the 1980s to the present, which is consistent with the climatic fluctuations of China, the Northern Hemisphere and Hengduan Mountains region, and these glaciers were steady or advanced when the climate was characterised by cold-dry and vice versa. The variational extent is different among 7 glaciers owing to the locations and scales. The ablation water equivalent of glacier tongue in Dagongba Glacier, Xiaogongba Glacier and Hailuogou Glacier is 2710 mm, 3139 mm and 5281 mm in 1982/83, respectively, and the mean value in Hailuogou Glacier is 6157 mm during 1990/91-97/98, which is 876 mm more than that in 1982/83. The ablation of Baishui Glacier No.1 was in decline with the rise of altitude owing to the less debris cover in the summer of 2002. Based on the mass observation during 2008.9.19-30, the glacier started to accumulate after October 6, and the accumulation depth is 1 cm equal to 5 mm water equivalent per day during 9.30-10.13.
LI Zong-xing,HE Yuan-qing,WANG Shi-jin,JIA Wen-xiong,HE Xian-zhong,Zhang Ning-ning,ZHU Guo-feng,PU Tao,DU Jian-kuo,XIN Hui-juan . Changes of Some Monsoonal Temperate Glaciers in Hengduan Mountains Region during 1900-2007[J]. Acta Geographica Sinica, 2009 , 64(11) : 1319 -1330 . DOI: 10.11821/xb200911004
[1] IPCC Report. Climate change 2007: Impacts, adaptation, and vulnerability. Summary for policymakers. Report of Working Group II of the Intergovernmental Panel on Climate Change. Cambridge: Cambridge University Press.
[2] China Meteorological Administration. Climate and Environment in China. Beijing: China Meteorological Press, 2006.
[中国气象局. 中国气候与环境演变. 北京: 气象出版社, 2006.]
[3] Yao Tandong, Liu Shiyin, Pu Jianchen et al. Recent glaciers retreating in High Asia and their impact on the water resources of Northwest China. Science in China: Series D, 2004, 34(6): 535-543.
[4] Pu Jianchen, Yao Tandong, Wang Ninglian et al. Fluctuations of the glaciers on the Qinghai-Tibetan Plateau during the past century. Journal of Glaciology and Geocryology, 2004, 26(5): 517-522.
[蒲建辰, 姚檀栋, 王宁练等. 近百年来青藏高原冰川的进退变化. 冰川冻土, 2004, 26(5): 517-522.]
[5] Ren Jiawen, Qin Dahe, Kang Shichang et al. Glaciers change and climate characterized by warm-dry in the middle Himalayas. Chinese Science Bulletin, 2003, 48(23): 2478-2482.
[任贾文, 秦大河, 康世昌等. 喜马拉雅山中段冰川变化及其气候暖干化特征. 科学通报, 2003, 48(23): 2478-2482.]
[6] Li Xin, Cheng Guodong, Jin Huijun et al. Cryospheric change in China. Global and Planetary Change, 2008, 62: 210-218.
[7] Pu Jianchen. Glacier Inventory of China (Changjiang River Drainage Basin). Lanzhou: Gansu Culture Press, 1994: 117-129.
[蒲健辰. 中国冰川目录(长江水系). 兰州: 甘肃文化出版社, 1994: 117-129.]
[8] Heim. The glaciation and soliefluction of Minya Gongkar. Geographical Journal, 1936, 87: 444-454.
[9] Li Jijun, Su Zhen. Glaciers of Hengduan Mountains. Beijing: Science Press, 1996.
[李吉均, 苏珍. 横断山冰川. 北京: 科学出版社, 1996.]
[10] Li Jijun.The field investigation of glaciers in Mt. Gongga//The Compilation of Field Investigation on Hengduan Mountains (1). Kunming: Yunnan People's Press, 1983.
[李吉均. 贡嘎山冰川考察//横断山考察专辑(1). 昆明: 云南人民出版社, 1983.]
[11] Li Jijun, Zheng Benxing, Yang Xijin et al. Glaciers in Tibet. Beijing: Science Press, 1986.
[李吉均, 郑本兴, 杨锡金等. 西藏冰川. 北京: 科学出版社, 1986.]
[12] Su Zhen, Liu Shiyin, Wang Ninglian et al. Glacier changes on the Hengduan Mountains and their response to climate// Zhong Xianghao//The Environment and Ecosystem in the Eastern Edge of the Qinghai-Xizang Plateau. Chengdu: Sichuan University Press, 2001: 102-109.
[苏珍, 刘时银, 王宁练等. 横断山冰川变化及其对气候波动的响应//钟祥浩//青藏高原东缘环境与生态. 成都: 四川大学出版社, 2001: 102-109.]
[13] Su Zhen, Shi Yafeng. The response of Chinese monsoonal temeperate glaciers to global warming since the Little Ice Age. Journal of Glaciology and Geocryology, 2000, 22(3): 223-228.
[苏珍, 施雅风. 小冰期以来中国海洋型冰川对全球变暖的响应. 冰川冻土, 2000, 22(3): 223-228.]
[14] Zhang Wenjing, Li Tongyang, Li Wei. Changes features of Hailuogou Glacier//Zhong Xianghao//Environment and Ecosystem in the Eastern Edge of Qinghai-Xizang Plateau. Chengdu: Sichuan University Press, 2001: 113-120.
[张文敬, 李同阳, 李伟. 海螺沟现代冰川对气候变化的响应//钟祥浩//青藏高原东缘环境与生态. 成都: 四川大学出版社,2001: 113-120.]
[15] He Yuanqing, Zhang Zhonglin, Pang Hongxi et al. Changing fetures of the climate and glaciers in China's monsoonal temperate glaciers region. Journal of Geophysical Research, 2003, 108(17): 1-7.
[16] Zheng Benxing, Zhao Xitao, Li Tiesong et al. Characteristcs and variation of Mingyong glacier in Mt. Meili. Journal of Glaciology and Geocryology, 1999, 21(2): 145-150.
[郑本兴, 赵希涛, 李铁松等. 梅里雪山明永冰川的特征与变化.冰川冻土, 1999, 21(2): 145-150.]
[17] Li Zongxing, He Yuanqing, Jia Wenxiong et al. Reponse of the "glaciers-runoff" system in a typical temperate-glacier, Hailuogou Glacier in Mt. Gongga of China, to global change. Scientia Geographica Sinica, 2008, 28(2): 229-234.
[李宗省, 何元庆, 贾文雄等. 我国海洋型冰川区“冰川－径流”系统的全球变化敏感性研究. 地理科学, 2008, 28(2): 229-234.]
[18] Li Zongxing, He Yuanqing, Yang Xiaomei et al. Changes of the Hailuogou Glacier, Mt. Gongga, China, against the background of climate change since the Holocene. Quaternary International, 2008, DOI: 10.1016/j.quaint.2008.09.005.
[19] Su Zhen, Liu Shiyin, Wang Ninglian et al. Studies of recent fluctuations of glacier length in the Gongga mountain//Xie Zichu, Kotlyakov V M//Glaciers and Environmental in the Qinghai-Xizang (Tibet) Plateau (1): The Gongga Mountain. Beijing: Science Press, 1994: 165-173.
[20] Song Bo. Application study in China's monsoonal temperate glacier region besed on GIS and remote sensing
[D].Beijing: Graduate University of Chinese Academy of Sciences, 2008.
[宋波. GIS 和遥感在我国海洋型冰川区的应用研究
[D]. 北京: 中国科学院研究生院, 2008.]
[21] Zhang Ningning, He Yuanqing, Pang Hongxi et al. The causes of glacier collapse in Mt. Yulong. Journal of Mountain Sciences, 2007, 25(4): 412-418.
[张宁宁, 何元庆, 庞洪喜等. 玉龙雪山冰川崩塌的原因. 山地学报, 2007, 25(4): 1329 64 卷地理学报412-418.]
[22] Li Zongxing, He Yuanqing, Jia Wenxiong et al. Change of Hailuogou Glacier during the past 100 years under the background of global warming. Journal of Glaciology and Geocryology, 2009, 31(1): 75-81.
[李宗省, 何元庆, 贾文雄等. 全球变暖影响下海螺沟冰川近百年变化的特征. 冰川冻土, 2009, 31(1): 75-81.]
[23] Wang Shaowu, Xie Zhihui, Chai Jingning et al. A study of the global average temperature in the last 1000 years. Progress in Natural Science, 2002, 12(11): 1145-1149.
[24] Wang Shaowu, Ye Jinlin, Gong Daoyi et al. Foundation of temperature change of China in the last 100 years. Journal of Applied Meteorological Science, 1998, 9(4): 392-400.
[王绍武, 叶瑾琳, 龚道溢等. 近百年中国气温序列的建立. 应用气象学报, 1998, 9(4): 392-400.]
[25] Fan Zexine, Achim Br?uning, Cao Kunfang et al. Annual temperature reconstruction in the central Hengduan Mountains, China, as deduced from tree rings. International Journal of Climatology, 2008, 28: 1879-1887.
[26] Fan Zexine, Achim Br?uning, Yang Bo et al. Tree ring density-based summer temperature reconstruction for the central Hengduan Mountains in southern China. Global and Planetary Change, 2008，DOI:10.1016/j.gloplacha.2008.10.001.
[27] Fan Zexine, Achim Br?uning, Cao Kunfang. Annual temperature reconstruction in the central Hengduan Mountains, China, as deduced from tree rings. Dendrochronologia, 2008, 26: 97-107.
[28] Yao Tandong, Duan Keqin, Tian Lide et al. Record of accmulation in Dasuopu ice core and the relationship with variation of the India summer monsoonal precipitation in the past 400years. Science in China: Series 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.]
[29] Gao Xiaoqing, Tao Maocang, Fen Song. The discussion in the relationship between glaciers change and climate change. Plateau Meteorology, 2000, 19(1): 9-16.
[高晓清, 汤懋苍, 冯松. 冰川变化与气候变化关系的若干探讨. 高原气象, 2000, 19(1): 9-16.]
/
| 〈 |
|
〉 |