OALib Journal期刊
ISSN: 2333-9721
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我国喜马拉雅山区冰湖扩张特征及其气候意义
DOI: 10.11821/xb201107003, PP. 895-904
Keywords: 喜马拉雅山区,冰湖面积扩张,垂直变化,气候效应
Abstract:
分析冰湖扩张特征和扩张方式及其气候意义,有利于认识冰川—冰湖—气候三者的变化关系和冰湖溃决灾害危险性程度。基于大比例尺地形图、DEM、ASTER影像等数据,分析近30年来我国喜马拉雅山区不同海拔高度冰湖变化的特征及冰湖—母冰川的相对位置的变化关系,探讨其气候效应。结果显示(1)存在冰湖的面积增大是冰湖面积扩张的主要贡献者,占总面积净增量的67%,新增湖的面积占总面积净增量的33%;(2)不同高度带冰湖面积多呈扩张态势,净增面积在5000~5300m出现峰值,指示气候变化的垂直差异性;(3)在2000s母冰川—冰湖距离为0的冰湖,数量占扩张冰湖总数的19%,而其冰湖面积增量却占了总面积增量的60%,为冰湖扩张的主体,反映出冰湖与母冰川关系越紧密,气候效应越强烈,冰湖面积增加越显著。
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