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西藏色林错湖面增长遥感信息动态分析
引用本文:杨日红,于学政,李玉龙.西藏色林错湖面增长遥感信息动态分析[J].国土资源遥感,2003,14(2):64-67.
作者姓名:杨日红  于学政  李玉龙
作者单位:1. 中国国土资源航空物探遥感中心,北京,100083
2. 中国地质调查局发展研究中心,北京,100083
摘    要:根据1972年陆地卫星MSS,1992年TM与1999年ETM+3个时相的遥感数据信息,对西藏色林错湖面增长进行动态分析后,发现近30a来湖面逐渐扩大,从1707km2增大到了1823km2.本文分别从气象学、构造地质学及高原隆升等方面分析了湖面扩大的原因.认为很有可能是由于温室效应,使得气温上升,冰雪、冰川融化和冻土软化释放水注入色林错,进而引起湖面增长.并就其所揭示的环境信息进行了初步探讨.

关 键 词:遥感信息  湖面扩大  动态监测  活动构造  西藏
文章编号:1001-070X(2003)02-0064-04
收稿时间:2002-09-20
修稿时间:2002年9月20日

THE DYNAMIC ANALYSIS OF REMOTE SENSING INFORMATION FOR MONITORING THE EXPANSION OF THE SELINCUO LAKE IN TIBET
YANG Ri-hong ,YU Xue-zheng ,LI Yu-long.THE DYNAMIC ANALYSIS OF REMOTE SENSING INFORMATION FOR MONITORING THE EXPANSION OF THE SELINCUO LAKE IN TIBET[J].Remote Sensing for Land & Resources,2003,14(2):64-67.
Authors:YANG Ri-hong  YU Xue-zheng  LI Yu-long
Institution:1. China Aero Geophysical Survey and Remote Sensing Center for Land and Resource, Beijing 100083, China;
2. Development &; Research Center, China Geological Survey, Beijing 100083, China
Abstract:According to the remote sensing data obtained in 1972,1992 and 1999, it is found that the Selincuo lake has expanded. The area of the lake has expanded from 1 707 km 2 to 1 823 km 2. Based on an analysis of such factors as meteorological phenomena, tectonic activity and uplifting of Qinghai-Tibet plateau, this paper explains the reasons for the lake expansion. It seems that the greenhouse effect plays the major role. With the rising of the temperature, the thawing of the glacier and the softening of the frozen earth result in the formation of free water, and then the water flows into the Selincuo Lake, leading to the expansion of the lake.
Keywords:Information of remote sensing  The enlargement of lake  Dynamic monitoring  Active structure  Tibet
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