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Ice Processes and Growth History on Arctic and Sub-Arctic Lakes Using ERS-1 SAR Data

机译:利用ERS-1 SAR数据的北极和亚北极湖冰过程和生长史

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摘要

A survey of ice growth and decay processes on a selection of shallow and deep sub-Arctic and Arctic lakes was conducted using radiometrically calibrated ERS-1 SAR images. Time series of radar backscatter data were compiled for selected sites on the lakes during the period ot ice cover (September to June) for the years 1991-1992 and 1992-1993. A variety of lake-ice processes could be observed, and significant changes in backscatter occurred from the time of initial ice formation in autumn until the onset of the spring thaw. Backscatter also varied according to the location and depth of the lakes. The spatial and temporal changes in backscatter were most constant and predictable at the shallow lakes on the North Slope of Alaska. As a consequence, they represent the most promising sites for long-term monitoring and the detection of changes related to global warming and its effects on the polar regions.
机译:使用辐射校准的ERS-1 SAR图像,对部分浅,深亚北极湖和北极湖的冰生长和衰减过程进行了调查。在1991-1992年和1992-1993年的冰盖期(9月至6月)内,为湖泊中选定的站点汇编了雷达后向散射数据的时间序列。可以观察到各种各样的湖冰过程,从秋季最初的冰层形成到春季解冻开始,反向散射发生了显着变化。反向散射也根据湖泊的位置和深度而变化。在阿拉斯加北坡的浅湖中,背向散射的时空变化最为稳定且可预测。因此,它们是长期监测和发现与全球变暖及其对极地的影响有关的变化的最有希望的场所。

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