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作 者:上官冬辉[1] 刘时银[1] 丁良福[1] 张世强[1] 李刚[1] 张勇[1] 李晶[1]
机构地区:[1]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,甘肃兰州730000
出 处:《冰川冻土》2008年第2期204-210,共7页Journal of Glaciology and Geocryology
基 金:国家重点基础研究发展计划(973计划)项目(2007CB411506);科技部基础支撑项目(2006FY110200);中国科学院知识创新工程重大项目(KZCX2-YW-301)资助
摘 要:运用多光谱遥感资料监测冰川变化已成为冰川研究的有效数据源,分析了念青唐古拉山脉西段念青唐古拉山峰区1970年冰川及Landsat ETM+(2000)解译的冰川分布.结果显示,念青唐古拉山峰区共有870条冰川,30a来冰川面积减小了5.7%,冰储量减少了7%;其中,冰川面积1~5km^2的冰川退缩的贡献最大,占总面积退缩量的56.7%.念青唐古拉山东南坡与西北坡的退缩幅度稍有不同,东南坡冰川面积减少了5.2%。西北坡冰川面积减少了6.9%.西北坡的拉弄冰川长度减少了(305±36)m,年退缩率为(10.2±1.2)m·a^-1,面积退缩为2.6%.当雄气象站的资料表明,冰川退缩主要受温度持续上升的影响,尤其是1985年以来的温度快速上升的影响.对处于西北坡冰川体积变化分析表明,冰川体积减少可能是导致纳木错湖水位上升、水量增加的重要因素.To monitor the glacier change by means of multi--spectrum remote sensing images provides a valid data bank. The Land ETM+ image was used to map the glacier distribution in 2000 by vision interpretation. Comparison of the glacier distribution maps from Glacier Inventory of China (1970) with those from Landsat ETM+(2000) reveals that the area and volume of 870 glaciers in the Nyainqentanglha Range has decreased 5.7 and 7%, respectively, in the recent 30 years; A- mong them, glaciers in the area rank of 1~ 5 km^2 contribute to 56.7% (19.5 km^2) of the total area loss. However, there is some difference between the southeast slopes and the northwest slopes of Nyainqentanglha Range. In the former glacier area reduced 5.2% and in the latter glacier area reduced 6.9 M. The Lanong Glacier in the northwest slope of Nyainqentanglha Range has retreated (305±36)m, with a retreat rate of (10.2±1.2)m·a^-1and an area shrinkage ratio of 2.6%. The records in Damxung Meteorological Station indicate that the glacier shrinkage was mainly subjected to continuous temperature rise, especially after 1985. In addition, decrease of glacier volume (1.115 km^3) in the northwest slopes of Nyainqentanglha Range results in the lake-level rising and water storage increasing (0. 765 km^3) of the Nam Lake.
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