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An Integrated Geospatial Approach to Monitoring the Bering Glacier System, Alaska

机译:一个集成的地理空间方法,用于监控白垩冰川系统,阿拉斯加

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The Bering Glacier is the largest and longest glacier in continental North America, with an area of approximately 5,175 km{sup}2, and a length of 190 km. It is also the largest surging glacier in America, having surged at least five times during the twentieth century. The last surge of the Bering Glacier occurred in 1993-1995, since then, the glacier has undergone constant and significant retreat thereby expanding the boundaries of Vitus Lake and creating a highly dynamic system, both ecologically and hydrologically. This study utilized GIS to integrate remote sensing observations, with detailed bathymetric, hydrographic and in situ water quality measurements of the rapidly expanding Vitus Lake. Vitus Lake has nearly doubled in surface area from 58.4 km{sup}2 to 108.8 km{sup}2, with a corresponding increase in water volume from 6.1 km{sup}3 to 10.5 km{sup}3 over the same period. The remote sensing observations were used to direct a systematic bathymetric, hydrographic and water quality measurement survey in Vitus Lake which revealed a complex three dimensional structure that is the result of sea water inflow, convection generated by ice melting and the injection of fresh water from beneath the glacier.
机译:Bering Glacier是北美大陆最大,最长的冰川,面积约为5,175公里{Sup} 2,长度为190公里。它也是美国最大的冰川冰川,在二十世纪至少飙升了五次。 Bering Glacier的最后一个浪涌发生在1993 - 1995年,从那时起,冰川经历了恒定而显着的撤退,从而扩大了Vitus Lake的界限,并在生态和水文中创造了高度动态的系统。本研究利用GIS整合遥感观察,详细的碱基,水文和原位水质测量的快速扩张的Vitus湖。 Vitus Lake在58.4 km {sup} 2至108.8 km {sup} 2的表面积下几乎翻了一番,在同一时期的6.1km {sup} 3至10.5公里} 3的水量相应增加。遥感观察用于指导vitus湖中的系统碱基,水文和水质测量调查,揭示了一种复杂的三维结构,这是海水流入的结果,由冰熔化产生的对流和从下方注入淡水冰川。

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