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首页> 外文期刊>Remote sensing in earth systems sciences >An Integrated Approach to Quantify Changes in NW Indian Himalayan Ice and Snow in Large Spatial Extent
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An Integrated Approach to Quantify Changes in NW Indian Himalayan Ice and Snow in Large Spatial Extent

机译:印度西北部喜马拉雅冰雪大范围变化量化的综合方法

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Abstract Monitoring spatio-temporal changes in glaciers and snow is important for estimating the impact of climate change in glaciated landscapes. The existing methods to map snow, ice, and debris-covered glaciers are complicated and have limitations. We introduce an integrated methodology to map the extent of total snow, isolated ice pockets together with the glaciers at the regional (megascopic) scale. In addition, we examined the sensitivity of the proposed methodology to different scales of mapping and datasets with different spatial resolutions (Landsat 8—30 m and Sentinel 2A—10 m). We implemented the approach in the five major river basins of Northwest India and developed an inventory for all the components of its glaciated area. All these data will help by providing inputs in hydrological models for assessing meltwater generated from the catchment. A change detection analysis in all these five river basins shows a maximum decrease in glacier and ice bodies by around 40 in the Ravi River basin to an overall 3 decrease in glacier and ice bodies in the Beas River basin over the past two and a half decades. The maximum loss in permanent snow cover is also in the Ravi River basin, whereas snow cover in the Yamuna River basin shows a slight increase. We also observed a rise in temperature, a recession of snowlines, and the emergence of glacial lakes in the region.
机译:摘要 冰川和积雪时空变化的监测对于预测气候变化对冰川景观的影响具有重要意义。现有的绘制雪、冰和碎屑覆盖的冰川的方法很复杂,而且有局限性。我们引入了一种综合方法,以绘制区域(大范围)尺度的总雪、孤立冰袋和冰川的范围。此外,我们研究了所提出的方法对不同比例的制图和具有不同空间分辨率的数据集(Landsat 8—30 m和Sentinel 2A—10 m)的敏感性。我们在印度西北部的五个主要河流流域实施了这种方法,并为其冰川区的所有组成部分制定了清单。所有这些数据都将通过为水文模型提供输入来评估集水区产生的融水,从而有所帮助。对这五个河流流域的变化检测分析显示,在过去二十五年中,拉维河流域的冰川和冰体最多减少了约40%,而比亚斯河流域的冰川和冰体总体减少了3%。永久性积雪损失最大的也是拉维河流域,而亚穆纳河流域的积雪略有增加。我们还观察到该地区的气温上升、雪线的衰退以及冰川湖的出现。

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