Spatio-temporal changes in the Machoi glacier Zanskar Himalaya India using geospatial technology

被引:17
|
作者
Taloor, Ajay Kumar [1 ]
Kothyari, Girish Chandra [2 ]
Manhas, Drinder Singh [1 ]
Bisht, Harish [3 ]
Mehta, Pankaj [4 ]
Sharma, Meenakshi [5 ]
Mahajan, Sugandha [5 ]
Roy, Sagarika [6 ]
Singh, Anil Kumar [7 ]
Ali, Sajid [8 ]
机构
[1] Univ Jammu, Dept Remote Sensing & GIS, Jammu 180006, India
[2] Inst Seismol Res, Gandhinagar 382007, Gujarat, India
[3] Kumaun Univ, Ctr Adv Study Geol, Naini Tal 263002, Uttarakhand, India
[4] Cent Univ Jammu, Dept Environm Sci, Bagla 181143, Jammu & Kashmir, India
[5] Govt Post Grad Coll Women, Dept Bot, Jammu 180003, India
[6] Indian Inst Sci, Dept Civil Engn, Bengaluru 560012, Karnataka, India
[7] DeHaat Agrevolut Private Ltd Gurugram, Harayana 122001, India
[8] Birbal Sahni Inst Palaeosci, Lucknow 226007, Uttar Pradesh, India
来源
关键词
Snout retreat; Glacier dynamics; Climate change; Zanskar Himalaya; Geospatial technology; GARHWAL-HIMALAYA; CLIMATE-CHANGE; GANGOTRI GLACIER; KARAKORAM-HIMALAYA; CHORABARI GLACIER; WINTER MONSOON; FLUCTUATIONS; RETREAT; BASIN; REGION;
D O I
10.1016/j.qsa.2021.100031
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
We present the temporal changes of Machoi glacier, Zanskar region of the north-western Himalaya, India using multi-temporal Landsat satellite data from 1973 to 2018. The results suggest that the Machoi glacier has retreated consistently from last 45 years with an uneven retreat rate. The temporal fluctuations since 1973 AD reveal that the glacier snout has retreated similar to 563 m at an average of similar to 12.51 m yr(-1). However, the snout has retreated at variable rates during different time intervals e.g., 80 m (average of similar to 11.43 m yr(-1)) from 1973 to 1980 AD, 120 m (average of similar to 12.0 m yr(-1)) from 1980 to 1990 AD, 123 m (average of similar to 12.3 m yr(-1)) from 1990 to 2000 AD, 128 m (average of similar to 12.8 m yr(-1)) from 2000 to 2010 AD and 112 m (average of similar to 14 m yr(-1)) from 2010 to 2018AD. The highest rate of snout (similar to 14 m yr(-1)) retreat during 2010-2018 AD is linked to the changing climate in the region as observed from the meteorological data. The analysis of meteorological data suggests that during this period temperature as well as the liquid precipitation have increased due to global warming whereas the extent of solid precipitation has decreased which might be the possible causes of higher retreat of Machoi glacier.
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页数:9
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