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Monitoring of moraine-dammed lakes: a remote sensing-based study in the Western Himalaya

机译:监测冰ora湖泊:在喜马拉雅山西部的遥感研究

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Monitoring of lakes in glaciated terrain in the Himalayan region has been recognized as one of the priority areas especially after the Kedarnath disaster. Among all types of glacial lakes, moraine dammed lakes (MDLs) are the most important from disaster point of view. Remote sensing plays a significant role in view of availability of unbiased repeated data on the expansion or contraction of MDLs located in rugged terrains of the Himalaya. Monitoring of two MDLs, associated with Katkar and Gepang-gath glaciers in Zanskar and Chandra sub-basins respectively was done using satellite images of 1965, 1976, 1989, 2001, 2006-07, 2012 and 2014. Survey of India (SOI) topographical maps of 1962 were also referred to monitor the respective glaciers lakes. SOI maps show the presence of only one lake associated with Gepang-gath glacier. Areal extent of the MDLs had increased from 21 to 57 ha between 1965 and 2014, and from 27 to 80 ha between 1962 and 2014 for the Katkar and Gepang-gath glaciers respectively. Increase in peak discharge of the two lakes was also estimated using different empirical models in case of outbursts of these lakes. The lake outburst probability for both these lakes was found to be very low (less than 1%), however, possibility of outburst of lakes due to natural calamity like cloud burst, landslide or earthquake cannot be ignored. The rate of retreat of these two glaciers was observed to be high due to the presence of MDLs in comparison to surrounding glaciers in the valley.
机译:喜马拉雅地区冰川地区湖泊的监测已被认为是重点领域之一,尤其是在吉达纳特灾难之后。从灾害的角度来看,在所有类型的冰川湖中,冰ora堰塞湖(MDL)是最重要的。鉴于在喜马拉雅山崎terrain地形中MDL扩展或收缩的无偏重复数据的可用性,遥感发挥了重要作用。分别使用1965、1976、1989、1989、2001、2006-07、2012和2014年的卫星图像对分别与Zanskar和Chandra子盆地的Katkar和Gepang-gath冰川相关的两个MDL进行了监测。印度(SOI)地形图还参考了1962年的地图来监视相应的冰川湖。 SOI地图显示只有一个与格庞加特冰川相关的湖泊。 1965年至2014年间,卡特卡冰川和盖邦盖特冰川的MDL面积从21公顷增加到57公顷,1962年至2014年从27公顷增加到80公顷。如果这两个湖泊爆发,也可以使用不同的经验模型来估算这两个湖泊的峰值流量增加。发现这两个湖泊的湖泊爆发概率都非常低(小于1%),但是,由于自然灾害(如云爆,滑坡或地震)而导致湖泊爆发的可能性不容忽视。与山谷中周围的冰川相比,由于存在MDL,这两个冰川的退缩率很高。

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