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A research of glacier change in West Kunlun through remote sensing

机译:西部昆仑冰川变化的遥感研究

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Glacier, due to the sensitivity to the climate change, has become an important indicator for global change research, especially the glaciers in the Arctic, Antarctic, and the third pole (Qinghai-Tibet plateau). Remote sensing, which has a capability to acquire the regional information of glaciers quickly, has become an effective tool to monitor and study the change of glaciers. In this paper, combining the NECP/NCAR reanalysis climatic data, the long time-series and continental area change of the glaciers and their melted lakes in West Kunlun with different watersheds were comparative analyzed by using LandSat TM/ETM+ images from 1991 to 2009, which is located in the northern margin of the Qinghai-Tibet plateau. The results show: 1) The total area of the glaciers in eastern West Kunlun reduced firstly then increased. Meanwhile the total area of the glaciers in western West Kunlun sustained decreased in recent 20 years. 2) There is a significant negative correlation between the area change of glaciers and the corresponding welted lakes in West Kunlun. 3) The area change difference of the glaciers in the eastern and western regions in West Kunlun is mainly induced by temperature.
机译:由于对气候变化敏感,冰川已成为全球变化研究的重要指标,尤其是北极,南极和第三极(青藏高原)的冰川。遥感具有快速获取冰川区域信息的能力,已经成为监测和研究冰川变化的有效工具。本文结合NECP / NCAR再分析气候资料,利用LandSat TM / ETM +影像从1991年至2009年对西昆仑冰川及其融化的湖泊在不同流域的长期时间序列和大陆面积变化进行了比较分析,它位于青藏高原的北缘。结果表明:1)西昆仑东部冰川总面积先减少后增加。同时,西昆仑西部的冰川总面积近20年持续减少。 2)西昆仑冰川与相应的湖水面积变化之间存在显着的负相关。 3)西昆仑东西部冰川面积变化差异主要是由温度引起的。

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