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作 者:WU Kun-peng LIU Shi-yin GUO Wan-qin WEI Jun-feng XU Jun-li BAO Wei-jia YAO Xiao-jun
机构地区:[1]State Key Laboratory of Cryospheric Sciences,Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Science,Lanzhou 730000,China [2]University of Chinese Academy of Sciences,Beijing 100049,China
出 处:《Journal of Mountain Science》2016年第8期1358-1374,共17页山地科学学报(英文)
基 金:supported by the fundamental program from the Ministry of Science and Technology of China(MOST)(Grant No.2013FY111400);the National Natural Science Foundation of China(Grant No.41190084);the MOST Technology Oriented Project(Grant No.2012BAC19B07);The second Chinese Glacier Inventory was a product of the previous MOST Project(Grant No.2006FY110200)
摘 要:Glaciers in the western Nyainqentanglha Range are an important source of water for social and economic development. Changes in their area were derived from two Chinese glacier inventories; one from the 197o 1:5o,ooo scale Chinese Topographic Maps series and the other from Landsat TM/ETM+ images acquired in 2009. Analyses also included boundaries from 2000 and 2014 Landsat TM/ETM+ images. A continuing and accelerating shrinkage of glaciers occurred here from 1970 to 2014, with glacier area decreasing by 244.38±29.48 km^2 (27.4%±3.3%) or 0.62%±0.08% a^-1. While this is consistent with a changing climate, local topographic parameters, such as altitude, slope, aspect and debris cover, are also important influences. Recession is manifested by a rise in the elevation of the glacier terminus. The shrinkage of glaciers with NE, N and NW orientations exceeded that of other aspects, and glaciers with SE and S orientations experienced less shrinkage. Changes in the average positive difference of glaciation (PDG) show that the western Nyainqentanglha Range has unfavorable conditions for glacier maintenance which is being exacerbated by a warming climate since 1970.
关 键 词:Glacier change Glacier inventory Western Nyainqentanglha Range Remote sensing
分 类 号:P343.6[天文地球—水文科学] P237[天文地球—地球物理学]
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