首页> 外文期刊>Current Science: A Fortnightly Journal of Research >Temporal changes in rate of recession: evidences from Satopanth and Bhagirath Kharak glaciers, Uttarakhand, using Total Station Survey.
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Temporal changes in rate of recession: evidences from Satopanth and Bhagirath Kharak glaciers, Uttarakhand, using Total Station Survey.

机译:衰退速度的时间变化:使用全站仪调查从北阿坎德邦的撒托潘特和巴吉拉特·卡拉克冰川提供的证据。

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摘要

Snouts of Satopanth and Bhagirath Kharak glaciers, located at the head of the Alaknanda valley in Chamoli District, Uttarakhand, were monitored using Total Station Survey. Retreat of the snouts and area vacated by recession of the glaciers were estimated for 44 years by way of superimposing the Survey of India toposheet of 1962 on the map prepared by Total Station Survey in 2006. The total area vacated by the Satopanth and Bhagirath Kharak glaciers during 44 years was 313,923.14 sq. m (0.314 sq. km) and 129,369.16 sq. m (0.13 sq. km) respectively. The annual average retreat of the snout of the Satopanth glacier between 1962 and 2005 (43 years) was estimated as 22.88 m/yr, whereas retreat was low (7.42 m/yr) for the Bhagirath Kharak glacier. Interestingly, actual field measurements for the year 2005-06, showed an estimated retreat of 6.5 and 1.5 m/yr for the Satopanth and Bhagirath Kharak glaciers respectively. Snouts of the Satopanth and Bhagirath Kharak glaciers recorded continuous recession for the past four decades, with decline in recession of both cases. Both glaciers are situated in the same basin and experience similar climatic conditions. However, different recession rates of glaciers are attributed to unequal distribution of tributary glaciers, active cirques, drainage characteristics, density and distribution of supraglacial debris over the glacier surface.
机译:使用全站仪监测对位于北阿坎德邦查莫里区Alaknanda谷头的Satopanth和Bhagirath Kharak冰川的口鼻进行了监测。通过将1962年印度地形调查叠加在2006年全站仪调查绘制的地图上,可以估算出鼻口的退缩和因冰川退缩而腾出的面积,为期44年。萨托潘特和巴吉拉特·哈拉克冰川腾出的总面积在44年中,分别为313,923.14平方米(0.314平方公里)和129,369.16平方米(0.13平方公里)。在1962年至2005年之间(43年),Satopanth冰川的口鼻部的年平均撤退量估计为22.88 m / yr,而Bhagirath Kharak冰川的撤退率较低(7.42 m / yr)。有趣的是,2005-06年的实际野外测量表明,Satopanth和Bhagirath Kharak冰川的后退估计分别为6.5和1.5 m / yr。在过去的40年中,Satopanth和Bhagirath Kharak冰川的口鼻部记录了持续的衰退,这两种情况的衰退都在减少。两种冰川都位于同一盆地,并经历相似的气候条件。然而,冰川退缩率的不同归因于支流冰川分布不均,活跃的旋流,排水特征,冰川表面碎屑的密度和分布。

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