Glacier mass loss in the Alaknanda basin, Garhwal Himalaya on a decadal scale

被引:14
作者
Remya, S. N. [1 ,2 ]
Kulkarni, Anil V. [1 ]
Hassan Syed, Tajdarul [2 ]
Nainwal, Harish Chandra [3 ]
机构
[1] Indian Inst Sci, Divecha Ctr Climate Change, Bangalore, Karnataka, India
[2] Indian Inst Technol ISM, Dept Appl Geol, Dhanbad, Bihar, India
[3] Hemvati Nandan Bahuguna Garhwal Univ, Srinagar, Uttarakhand, India
关键词
Alaknanda Basin; debris thickness; geodetic method; mass budget; Satopanth Glacier; BHAGIRATH-KHARAK GLACIERS; DEBRIS COVER; GANGOTRI GLACIER; WESTERN HIMALAYA; MILAM GLACIER; BALANCE; RECESSION; REGION; ELEVATION; MODELS;
D O I
10.1080/10106049.2020.1844309
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Himalayan glaciers significantly contribute to the largest river systems like the Indus, Ganga, and the Brahmaputra. The change in glacial area and mass can affect the mountain community and people living in the Indo-Gangetic plain. The present study adopted the geodetic method to estimate the elevation change and mass budget of 61 glaciers in the Alaknanda Basin, using the satellite data of Cartosat-1 (2011, 2014, 2017) and SRTM (2000). Besides, the DEM of 1962 (SOI Toposheet) and 2000 (SRTM) is used to estimate the mass budget of Satopanth (SPG) and Bhagirath Kharak glaciers (BKG). The field debris thickness of SPG (2015-2017) is compared with the elevation change (2000-2017). Further, we have compared the mass loss of the glaciers with their volume. The results suggest the sustained mass loss of 1.85 +/- 0.10 Gt out of 33.9 +/- 8.8 Gt for 61 glaciers in the basin from 2000-2017. The mass loss of SPG and BKG during 2000-2017 is 0.20 +/- 0.02 Gt and 0.24 +/- 0.03 Gt, whereas from 1962 to 2000, is 0.083 +/- 0.03 Gt and 0.091 +/- 0.04 Gt, respectively. The analysis facilitates a better understanding of glacier mass changes in the Alaknanda basin on a multi-decadal scale.
引用
收藏
页码:3014 / 3032
页数:19
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