近50年来中国天山冰川面积变化对气候的响应

doi:10.11821/xb201101004

地理学报 ›› 2011, Vol. 66 ›› Issue (1): 38-46.doi: 10.11821/xb201101004

近50年来中国天山冰川面积变化对气候的响应

王圣杰¹, 张明军^1,2, 李忠勤^2,1, 王飞腾², 李慧林², 李亚举¹, 黄小燕¹

1. 西北师范大学地理与环境科学学院，兰州730070;
2. 中国科学院寒区旱区环境与工程研究所冰冻圈科学国家重点实验室/天山冰川观测试验站，兰州730000

收稿日期:2010-08-16 修回日期:2010-09-29 出版日期:2011-01-25 发布日期:2011-01-25
通讯作者: 张明军(1975-), 男, 博士, 教授, 主要从事冰川与环境研究。E-mail: mjzhang2004@163.com
作者简介:王圣杰(1987-), 男, 硕士生, 主要从事全球变化与冰川研究。E-mail: geowang@126.com
基金资助:
国家自然科学基金项目(40701035; 40631001; 40571033; 40701034; J0630966); 教育部新世纪优秀人才支持计划项目(NCET-10-0019); 陇原青年创新人才扶持计划项目; 国家重点基础研究发展规划(973) 项目(2010CB951003; 2007CB411501); 中国科学院知识创新工程重要方向项目(KZCX2-YW-127); 冰冻圈科学国家重点实验室自主研究项目; 西北师范大学知识与科技创新工程创新团队项目(NWNU-KJCXGC-03-66)

Response of Glacier Area Variation to Climate Change in Chinese Tianshan Mountains in the Past 50 Years

WANG Shengjie¹, ZHANG Mingjun^1,2, LI Zhongqin^2,1, WANG Feiteng², LI Huilin², LI Yaju¹, HUANG Xiaoyan¹

1. College of Geography and Environment Sciences, Northwest Normal University, Lanzhou 730070, China;
2. State Key Laboratory of Cryospheric Sciences/Tianshan Glaciological Station, Cold and Arid Regions Environmental and Engineering Research Institute, CAS, Lanzhou 730000, China

Received:2010-08-16 Revised:2010-09-29 Online:2011-01-25 Published:2011-01-25
Supported by:
National Natural Science Foundation of China, No.40701035; No.40631001; No.40571033; No.40701034; No.J0630966; The Program for New Century Excellent Talents in University by the Ministry of Education of China, No.NCET-10-0019; The Foundation for Young Innovative Scientists in Gansu Province; The National Basic Research Program of China, No.2010CB951003; No.2007CB411501; The Knowledge Innovation Project of Chinese Academy of Sciences, No.KZCX2-YW-127; The Independent Research Program of State Key Laboratory of Cryospheric Sciences of Chinese Academy of Sciences; The Knowledge and Technological Innovation Project of Northwest Normal University, No.NWNU-KJCXGC-03-66

摘要/Abstract

摘要： 基于1960 年以来中国天山各流域冰川面积变化的统计分析，系统地研究了中国天山冰川面积变化对气候的响应情况。结果表明，近50 年来中国天山冰川的面积缩小了11.5%，对研究时段统一化后发现面积年均退缩率为0.31% a^-1。各流域冰川面积退缩速度存在一定差异，但冰川加速消融趋势明显。天山地区14 个气象站的气温与降水量倾向率平均值分别为0.34 ^oC·(10 a)^-1与11 mm·(10 a)^-1，气温在干季增幅大而在湿季增幅略小，降水量在干季增长缓慢而在湿季增长显著，这样的气候变化趋势有助于天山冰川的退缩。

关键词: 天山, 冰川变化, 冰川面积, 气候变化

Abstract: Based on the statistics of glacier area variation measured in Chinese Tianshan Mountains since 1960, the response of glacier area variation to climate change is discussed systematically. Results show that the total area of the glaciers has reduced by 11.5% in the past 50 years, which is a weighted percentage according to the glacier areas of 10 drainage areas divided by Glacier Inventory of China. The annual percentage of area changes (APAC) of glaciers in the Tianshan Mountains is 0.31% , after the standardization of the study period. According to the 14 meteorological stations in the Tianshan Mountains, both the temperature and precipitation display a marked increasing tendency from 1960 to 2009 with a rate of 0.34 ℃· (10 a)^-1 and 11 mm·(10 a)^-1, respectively. The temperature in dry seasons (from November to March) increases rapidly with a rate of 0.46 ℃·(10 a)^-1, but the precipitation grows slowly at 2.3 mm·(10 a)^-1; while the temperature in wet seasons (from April to October) grows with a rate of 0.25 ℃·(10 a)^-1, but the precipitation increases at 8.7 mm·(10 a)^-1.

Key words: Tianshan Mountains, glacier variation, glacier area, climate change

王圣杰, 张明军, 李忠勤, 王飞腾, 李慧林, 李亚举, 黄小燕. 近50年来中国天山冰川面积变化对气候的响应[J]. 地理学报, 2011, 66(1): 38-46.

WANG Shengjie, ZHANG Mingjun, LI Zhongqin, WANG Feiteng, LI Huilin, LI Yaju, HUANG Xiaoyan. Response of Glacier Area Variation to Climate Change in Chinese Tianshan Mountains in the Past 50 Years[J]. Acta Geographica Sinica, 2011, 66(1): 38-46.

参考文献

[1] Liu Chaohai. Glacier resources and distributive characteristics in the Central Asia Tianshan Mountains. Journal ofGlaciology and Geocryology, 1995, 17(3): 193-203. [刘潮海. 中亚天山冰川资源及其分布特征. 冰川冻土, 1995, 17(3):193-203.]

[2] Li Baolin, Zhu Axing, Zhang Yichi et al. Glacier change over the past four decades in the middle Chinese Tien Shan.Journal of Glaciology, 2006, 52(178): 425-432.

[3] Aizen V B, Kuzmichenok V A, Surazakov A B et al. Glacier changes in the central and northern Tien Shan during the last140 years based on surface and remote-sensing data. Annals of Glaciology, 2006, 43(1): 202-213.

[4] Bolch T. Climate change and glacier retreat in northern Tien Shan (Kazakhstan/Kyrgyzstan) using remote sensing data.Global and Planetary Change, 2007, 56(1-2): 1-12.

[5] Kutuzov S. Glacier retreat and climatic variability in the eastern Terskey-Alatoo, inner Tien Shan between the middle of the19th century and beginning of the 21st century. Global and Planetary Change, 2009, 69(1/2): 59-70.

[6] Narama C, Kaab A. Spatial variability of recent glacier area changes in the Tien Shan Mountains, Central Asia, usingCorona (~1970), Landsat (~2000), and ALOS (~2007) satellite data. Global and Planetary Change, 2010, 71(1-2): 42-54.

[7] Haeberli W, Hoelzle M, Paul F et al. Integrated monitoring of mountain glaciers as key indicators of global climate change:the European Alps. Annals of Glaciology, 2007, 46(1): 150-160.

[8] Hoelzle M, Chinn T, Stumm D et al. The application of glacier inventory data for estimating past climate change effects onmountain glaciers. Global and Planetary Change, 2007, 56(1-2): 69-82.

[9] Wu Yanhong, Zhu Liping. The response of lake-glacier variations to climate change in Nam Co Catchment, central TibetanPlateau, during 1970-2000. Journal of Geographical Sciences, 2008, 18(2): 177-189.

[10] Li Zongxing, He Yuanqing, Wang Shijin et al. Changes of some monsoonal temperate glaciers in Hengduan MountainsRegion during 1900-2007. Acta Geographica Sinica, 2009, 64(11): 1319-1330. [李宗省, 何元庆, 王世金等. 1900-2007 年横断山区部分海洋型冰川变化. 地理学报, 2009, 64(11): 1319-1330.]

[11] Bolch T, Menounos B, Wheate R. Landsat-based inventory of glaciers in western Canada, 1985-2005. Remote Sensing ofEnvironment, 2010, 114(1): 127-137.

[12] Nie Yong, Zhang Yili, Liu Linshan et al. Glacial change in the vicinity of Mt. Qomolangma (Everest), central highHimalayas since 1976. Journal of Geographical Sciences, 2010, 20(5): 667-686.

[13] Hu Ruji. Physical Geography of the Tianshan Mountains in China. Beijing: China Environmental Science Press, 2004:1-14, 180-198. [胡汝骥. 中国天山自然地理. 北京：中国环境科学出版社, 2004: 1-14, 180-198.]

[14] Shi Yafeng. Glaciers and Related Environments in China. Beijing: Science Press, 2008: 42-51.

[15] Ren Binghui. Existing glacier fluctuation and its relation to the climatical changes in China. Journal of Glaciology andGeocryology, 1988, 10(3): 244-249. [任炳辉. 我国现代冰川变化及其与气候变化的关系. 冰川冻土, 1988, 10(3):244-249.]

[16] Li Zhongqin, Han Tianding, Jing Zhefan et al. A summary of 40-year observed variation facts of climate and Glacier No.1at headwater of Urumqi River, Tianshan, China. Journal of Glaciology and Geocryology, 2003, 25(2): 117-123. [李忠勤,韩添丁, 井哲帆等. 乌鲁木齐河源区气候变化和1 号冰川40 a观测事实. 冰川冻土, 2003, 25(2): 117-123.]

[17] Ding Yongjian, Liu Shiyin, Li Jing et al. The retreat of glaciers in response to recent climate warming in western China.Annals of Glaciology, 2006, 43(1): 97-105.

[18] Li Zhongqin, Li Kaiming, Wang Lin. Study on recent glacier changes and their impact on water resources in Xinjiang,Northwestern China. Quaternary Sciences, 2010, 30(1): 96-106. [李忠勤, 李开明, 王林. 新疆冰川近期变化及其对水资源的影响研究. 第四纪研究, 2010, 30(1): 96-106.]

[19] Wang Yetang, Hou Shugui, Liu Yaping. Glacier changes in the Karlik Shan, eastern Tien Shan, during 1971/72-2001/02.Annals of Glaciology, 2010, 50(53): 39-45.

[20] Yao Yonghui, Li Huiguo, Zhang Baiping. Glacier changes in the past 30 years at the east watershed of Mt. Tomor. AridLand Geography, 2009, 32(6): 828-833. [姚永慧, 励惠国, 张百平. 近30 年来天山托木尔峰东侧分水岭处冰川变化. 干旱区地理, 2009, 32(6): 828-833.]

[21] Wang Xin, Xie Zichu, Li Qiaoyuan et al. Sensitivity analysis of glacier systems to climate warming in China. Journal ofGeographical Sciences, 2008, 18(2): 190-200.

[22] Liu Chaohai, Kang Ersi, Liu Shiyin et al. Study on the glacier variation and its runoff responses in the arid region ofNorthwest China. Science in China: Series D, 1999, 42(suppl.): 64-71.

[23] Liu Shiyin, Ding Yongjian, Shangguan Donghui et al. Glacier retreat as a result of climate warming and increasedprecipitation in the Tarim River Basin, Northwest China. Annals of Glaciology, 2006, 43(1): 91-96.

[24] Kang Ersi. A study on changes of the glacier system and its runoff at the north flank of the Tianger Mountain in theTianshan Mountains. Journal of Glaciology and Geocryology, 1996, 18(suppl.): 60-74. [康尔泗. 天山天格尔山北坡冰川系统及其径流变化研究. 冰川冻土, 1996, 18(增刊): 60-74.]

[25] Chen Jianming, Liu Chaohai. Application of the repeated aerial photogrammetry to monitoring glacier variation in thedrainage area of the Urumqi River. Journal of Glaciology and Geocryology, 1996, 18(4): 331-336. [陈建明, 刘潮海. 重复航空摄影测量方法在乌鲁木齐河流域冰川变化监测中的应用. 冰川冻土, 1996, 18(4): 331-336.]

[26] Wang Shuhong, Xie Zichu, Li Qiaoyuan. Comparison study of glacier variations in East and West Tianshan Mountains.Journal of Glaciology and Geocryology, 2008, 30(6): 946-953. [王淑红, 谢自楚, 李巧媛. 近期东西天山冰川变化的对比研究. 冰川冻土, 2008, 30(6): 946-953.]

[27] Jia Wenxiong, He Yuanqing, Li Zongxing et al. The regional difference and catastrophe of climatic change in Qilian Mt.Region. Acta Geographica Sinica, 2008, 63(3): 257-269. [贾文雄, 何元庆, 李宗省等. 祁连山区气候变化的区域差异特征及突变分析. 地理学报, 2008, 63(3): 257-269.]

[28] Li Zongxing, He Yuanqing, Xin Huijuan et al. Spatio-temporal variations of temperature and precipitation in Mts.Hengduan Region during 1960-2008. Acta Geographica Sinica, 2010, 65(5): 563-579. [李宗省, 何元庆, 辛惠娟等. 我国横断山区1960-2008 年气温和降水时空变化特征. 地理学报, 2010, 65(5): 563-579.]

[29] Duan Jianping, Wang Lily, Ren Jiawen et al. Progress in glacier variations in China and its sensitivity to climatic changeduring the past century. Progress in Geography, 2009, 28(2): 231-237. [段建平, 王丽丽, 任贾文等. 近百年来中国冰川变化及其对气候变化的敏感性研究进展. 地理科学进展, 2009, 28(2): 231-237.]

[30] Kang Ersi. Glacier-snow Water Resources and Mountain Runoff in the Arid Area of Northwest China. Beijing: SciencePress, 2002: 33-37. [康尔泗. 中国西北干旱区冰雪水资源与出山径流. 北京: 科学出版社, 2002: 33-37.]

[31] Gao Xiaoqing, Tang Maocang. Discussion on the relationship between glacial fluctuation and climate change. PlateauMeteorology, 2000, 19(1): 9-16. [高晓清, 汤懋苍. 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.]

[32] Liu Bo. Characteristics of climate changes in Xinjiang from 1960 to 2005. Climatic and Environmental Research, 2009,14 (4): 414-426. [刘波. 1960~2005 年新疆气候变化的基本特征. 气候与环境研究, 2009, 14 (4): 414-426.]

[33] Wang Ninglian. Mountain glacier fluctuations and climatic change during the last 100 years. Journal of Glaciology andGeocryology, 1992, 14(3): 242-250. [王宁练. 近百年来山地冰川波动与气候变化. 冰川冻土, 1992, 14(3): 242-250.]

[34] Dyurgerov M B, Meier M F. Twentieth century climate change: Evidence from small glaciers. Proceedings of the NationalAcademy of Sciences of the United States of America, 2000, 97(4): 1406-1411.

[35] Li Zhongqin, Wang Wenbin, Wang Feiteng. Characteristics of ionic concentration and δ18O and their variability indry-season and wet-season snow on Urumqi glacier No.1, eastern Tien Shan. Annals of Glaciology, 2008, 49(1): 217-223.

[36] Ye Baisheng, Ding Yongjian, Liu Chaohai. Response of valley glaciers in various sizes and their runoff to climate change.Journal of Glaciology and Geocryology, 2001, 23(2): 103-110. [叶柏生, 丁永建. 刘潮海. 不同规模山谷冰川及其径流对气候变化的响应过程. 冰川冻土, 2001, 23(2): 103-110.]

[37] Ding Yongjian. Global glacial fluctuations in response to climatic change in the past 40 a. Science in China(Series D),1996, 39(1): 66-73.

[38] Shi Yafeng, Liu Chaohai, Kang Ersi. The Glacier Inventory of China. Annals of Glaciology, 2010, 50(53): 1-4.

近50年来中国天山冰川面积变化对气候的响应

Response of Glacier Area Variation to Climate Change in Chinese Tianshan Mountains in the Past 50 Years

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