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Compiling an Inventory of Glacier-Bed Overdeepenings and Potential New Lakes in De-Glaciating Areas of the Peruvian Andes: Approach, First Results, and Perspectives for Adaptation to Climate Change

机译:编制秘鲁安第斯山脉无冰川地区冰川床加深层和潜在新湖泊的清单:方法,初步结果和适应气候变化的观点

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Global warming causes rapid shrinking of mountain glaciers. New lakes can, thus, form in the future where overdeepenings in the beds of still-existing glaciers are becoming exposed. Such new lakes can be amplifiers of natural hazards to downstream populations, but also constitute tourist attractions, offer new potential for hydropower, and may be of interest for water management. Identification of sites where future lakes will possibly form is, therefore, an essential step to initiate early planning of measures for risk reduction and sustainable use as part of adaptation strategies with respect to impacts from climate change. In order to establish a corresponding knowledge base, a systematic inventory of glacier-bed overdeepenings and possible future lakes was compiled for the still glacierized parts of the Peruvian Andes using the 2003–2010 glacier outlines from the national glacier inventory and the SRTM DEM from the year 2000. The resulting inventory contains 201 sites with overdeepened glacier beds >1 ha (10 4 m 2 ) where notable future lakes could form, representing a total volume of about 260 million m 3 . A rough classification was assigned for the most likely formation time of the possible new lakes. Such inventory information sets the stage for analyzing sustainable use and hazard/risk for specific basins or regions.
机译:全球变暖导致高山冰川迅速萎缩。因此,将来可能会形成新的湖泊,在那里仍然存在的冰川床中的过度加深现象将逐渐暴露出来。这样的新湖泊可以成为对下游人口的自然灾害的加剧者,但也可以构成旅游胜地,为水力发电提供新的潜力,并且可能对水资源管理产生兴趣。因此,确定可能形成未来湖泊的地点是启动早期计划以降低风险和可持续利用措施的重要步骤,作为适应战略应对气候变化影响的一部分。为了建立相应的知识库,使用了国家冰川清单中的2003-2010年冰川轮廓线和秘鲁冰川中的SRTM DEM,为秘鲁安第斯山脉仍在冰川化的部分编制了系统的冰川床加深和可能的未来湖泊清单。年份为2000年。由此产生的清单包含201个站点,其中加深的冰川床> 1公顷(10 4 m 2),未来可能形成明显的湖泊,总量约为2.6亿m 3。对可能出现的新湖泊的最可能形成时间进行了粗略分类。此类清单信息为分析特定流域或区域的可持续利用和危害/风险奠定了基础。

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