Applicability of an ultra-long-range terrestrial laser scanner to monitor the mass balance of Muz Taw Glacier, Sawir Mountains, China

被引:11
|
作者
Wang, FeiTeng [1 ]
Xu, ChunHai [1 ,2 ]
Li, ZhongQin [1 ]
Anjum, Muhammad Naveed [1 ,2 ]
Wang, Lin [1 ]
机构
[1] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Cryospher Sci, Tien Shan Glaciol Stn, Lanzhou 730000, Gansu, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
来源
SCIENCES IN COLD AND ARID REGIONS | 2018年 / 10卷 / 01期
基金
中国国家自然科学基金;
关键词
glacier front variation; geodetic mass balance; Riegl VZ (R)-6000 terrestrial laser scanner; Muz Taw Glacier; Sawir Mountains;
D O I
10.3724/SP.J.1226.2018.00047
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Glacier mass balance is a key component of glacier monitoring programs. Information on the mass balance of Sawir Mountains is poor due to a dearth of in-situ measurements. This paper introduces the applicability of an ultra-long-range terrestrial laser scanner (TLS) to monitor the mass balance of Muz Taw Glacier, Sawir Mountains, China. The Riegl VZ (R)-6000 TLS is exceptionally well-suited for measuring snowy and icy terrain. Here, we use TLS to create repeated high spatiotemporal resolution DEMs, focusing on the annual mass balance (June 2, 2015 to July 25, 2016). According to TLS-derived high spatial resolution point clouds, the front variation (glacier retreat) of Muz Taw Glacier was 9.3 m. The mean geodetic elevation change was 4.55 m at the ablation area. By comparing with glaciological measurements, the glaciological elevation change of individual stakes and the TLS-derived geodetic elevation change of corresponding points matched closely, and the calculated balance was -3.864 +/- 0.378 m w.e.. This data indicates that TLS provides accurate results and is therefore suitable to monitor mass balance evolution of Muz Taw Glacier.
引用
收藏
页码:47 / 54
页数:8
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