Quantifying ice storage in upper Indus river basin using ground-penetrating radar measurements and glacier bed topography model version 2
Zou, Xiaojuan3,4; Gao, Haifeng3,5; Zhang, Yinsheng1,3; Ma, Ning2; Wu, Jianfeng3,4; Farhan, Suhaib Bin6
刊名HYDROLOGICAL PROCESSES
2021-04-01
卷号35期号:4页码:14
关键词glacier bed topography version 2 ground‐ penetrating radar ice reserve ice thickness optimal parametric scheme upper Indus river basin
ISSN号0885-6087
DOI10.1002/hyp.14145
通讯作者Zhang, Yinsheng(yszhang@itpcas.ac.cn)
英文摘要Ice reserve estimates is a fundamental prerequisite for water resources management. We selected the UIB (upper Indus river basin) as study area because it contains the most abundant mid-latitude glaciers outside the polar region, however, the ice reserve estimates remain unclear due to the harsh topography. In this study, we validated the parameters of the GlabTop2 model (Glacier Bed Topography version 2) using the ice thickness measured by GPR (ground-penetrating radar) and compared the "GPR-measured ice thickness and ice bed elevation" versus "the estimated results obtained from GlabTop2." Integrated with IDW (inverse distance weighted) interpolated results of glaciers of various sizes, a reasonable parametric scheme (tau = 120 kPa and f = 0.8) of GlabTop2 was applied on vast amounts of glaciers in the UIB region. The GlabTop2 estimates indicated that the ice thickness of the UIB varied from 0 to 736.0 +/- 110.0 m, with an average value of 74.5 +/- 11.2 m. A significant spatial heterogeneity exists in the sub-basins. The Shyok, Shigar and Hunza that contain the most abundant ice reserve. Lesser quantities are stored in the Western Himalaya and Hindu Kush ranges, which account for 11.3 % and 6.7 % of the total ice reserve in the UIB, respectively. A total volume of 1162.4 +/- 175.1 km(3) of glacier can be converted to 1046.2 +/- 157.6 Gt ice reserve; this is 13.6 times the annual average discharge obtained from the outlet of the Besham hydrological station. We aim to present estimates that can provide the baseline information for glaciology study of the Indus river.
资助项目Key International Project of International Cooperation Bureau of CAS[131C11KYSB20160061] ; National Key Research and Development Program of China[2017YFA0603101] ; National Natural Science Foundation of China[41661144025] ; Strategic Priority Research Program (A), CAS[XDA20060202]
WOS关键词DEBRIS-COVERED GLACIERS ; CHHOTA SHIGRI GLACIER ; KARAKORAM HIMALAYA ; CLIMATE-CHANGE ; THICKNESS ; VOLUME
WOS研究方向Water Resources
语种英语
出版者WILEY
WOS记录号WOS:000645220700005
资助机构Key International Project of International Cooperation Bureau of CAS ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; Strategic Priority Research Program (A), CAS
内容类型期刊论文
源URL[http://ir.igsnrr.ac.cn/handle/311030/162905]  
专题中国科学院地理科学与资源研究所
通讯作者Zhang, Yinsheng
作者单位1.China Pakistan Joint Res Ctr Earth Sci, Islamabad, Pakistan
2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing, Peoples R China
3.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing, Peoples R China
4.Univ Chinese Acad Sci, Beijing, Peoples R China
5.Minist Ecol & Environm, Satellite Applicat Ctr Ecol & Environm, Beijing, Peoples R China
6.Pakistan Space & Upper Atmosphere Res Commiss, Space Applicat & Res Wing, Karachi, Pakistan
推荐引用方式
GB/T 7714
Zou, Xiaojuan,Gao, Haifeng,Zhang, Yinsheng,et al. Quantifying ice storage in upper Indus river basin using ground-penetrating radar measurements and glacier bed topography model version 2[J]. HYDROLOGICAL PROCESSES,2021,35(4):14.
APA Zou, Xiaojuan,Gao, Haifeng,Zhang, Yinsheng,Ma, Ning,Wu, Jianfeng,&Farhan, Suhaib Bin.(2021).Quantifying ice storage in upper Indus river basin using ground-penetrating radar measurements and glacier bed topography model version 2.HYDROLOGICAL PROCESSES,35(4),14.
MLA Zou, Xiaojuan,et al."Quantifying ice storage in upper Indus river basin using ground-penetrating radar measurements and glacier bed topography model version 2".HYDROLOGICAL PROCESSES 35.4(2021):14.
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