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作 者:YAO TanDong LI ZhiGuo YANG Wei GUO XueJun ZHU LiPing KANG ShiChang WU YanHong YU WuSheng
机构地区:[1]Key Laboratory of Tibetan Environment Changes & Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China [2]State Key Laboratory of Cryosphere, Chinese Academy of Sciences, Lanzhou 730000, China [3]Key Laboratory of Digital Earth Sciences, Center for Earth Observation and Digital Earth, Chinese Academy of Sciences, Beijing 100190, China
出 处:《Chinese Science Bulletin》2010年第20期2072-2078,共7页
基 金:supported by the Ministry of Science and Technology of the People's Republic of China(2005CB422004);the National Natural Science Foundation of China(40810019001);BRAHMATWINN (FP6-036952);the Program of Tibet Science and Technology Agency
摘 要:Glaciers in the Yarlung Zangbo River witness severe glacial retreat nowadays,which gives important influence on lake processes in the region.We have studied glacial distribution,glacial mass balance and found large deficit in glacial mass and its impact in the region.Our study also integrated the variation in glacial-fed lakes of the Nam Co and Ranwu Lake,and presented an initial assessment of the impact of glacial mass balance on lakes.The study has shown a significant contribution of glacial melting to recent lake expansion and lake level rising.Glaciers in the Yarlung Zangbo River witness severe glacial retreat nowadays, which gives important influence on lake processes in the region. We have studied glacial distribution, glacial mass balance and found large deficit in glacial mass and its impact in the region. Our study also integrated the variation in glacial-fed lakes of the Nam Co and Ranwu Lake, and presented an initial assessment of the impact of glacial mass balance on lakes. The study has shown a significant contribution of glacial melting to recent lake expansion and lake level rising.
关 键 词:冰川物质平衡 冰川分布 雅鲁藏布江 湖泊变化 冰川退缩 冰川融化 纳木错 上升
分 类 号:P343.6[天文地球—水文科学] P588.1[天文地球—地球物理学]
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