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An Analysis of Past and Future Changes in the Ice Cover of Two High-Arctic Lakes Based on Synthetic Aperture Radar (SAR) and Landsat Imagery

机译:基于合成孔径雷达(saR)和Landsat影像的两个高北极湖泊冰盖过去和未来变化分析

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摘要

Space-borne remotely sensed data can provide valuable insight into cryospheric processes in remote high-latitude regions for which direct observations are limited. In this study we use synthetic aperture radar (SAR) and Landsat imagery to evaluate recent changes in the ice cover of Upper and Lower Murray Lakes (81°20′N, 69°30′W) on Ellesmere Island, Nunavut, Canada. These data highlight changes in ice conditions that have occurred over the past decade and provide a means for assessing the likely impacts of rising temperatures on future lake-ice conditions. Under current (1997–2007) climatic conditions the Murray Lakes average several weeks of ice-free conditions in August and early September, although in some years a partial ice cover persists throughout the year. The observed relationship between summer temperature and ice melt at Upper and Lower Murray Lakes suggests that recent warming in the High Arctic has forced the lakes near a threshold from a state characterized by perennial ice cover to the current state that includes seasonal melting of lake ice. Projected future warming will significantly increase the duration of ice free conditions on Upper and Lower Murray Lakes, with ice-out predicted to occur 13.5 ± 4.0 and 17.6 ± 5.6 days earlier, respectively, for every 1 °C increase in mean June–July temperature.
机译:星载遥感数据可提供对直接观测有限的偏远高纬度地区冰冻圈过程的宝贵见解。在这项研究中,我们使用合成孔径雷达(SAR)和Landsat影像来评估加拿大努纳武特岛Ellesmere岛上墨累湖和下墨累湖(81°20′N,69°30′W)的冰盖变化。这些数据强调了过去十年来冰情的变化,并提供了一种评估温度升高对未来湖冰状况可能影响的手段。在当前(1997-2007年)气候条件下,默里湖在8月和9月初平均无冰期数周,尽管在某些年份中全年仍会部分覆冰。观测到的夏季温度与上墨累湖和下墨累湖和下墨累湖之间的冰融化之间的关系表明,高北极地区最近的变暖迫使湖泊接近阈值,从以多年生冰覆盖为特征的状态到当前包括湖冰的季节性融化的状态。预计未来的变暖将显着增加默里湖上和下湖无冰条件的持续时间,预计6月至7月平均温度每升高1°C,结冰时间分别提前13.5±4.0和17.6±5.6天。 。

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