Vertical and horizontal surface displacements near Jakobshavn Isbrae driven by melt-induced and dynamic ice loss

被引:26
作者
Nielsen, Karina [1 ]
Khan, Shfaqat A. [1 ]
Spada, Giorgio [2 ]
Wahr, John [3 ,4 ]
Bevis, Michael [5 ]
Liu, Lin [6 ]
van Dam, Tonie [7 ]
机构
[1] Tech Univ Denmark, DTU Space Natl Space Inst, Dept Geodesy, DK-2800 Lyngby, Denmark
[2] Univ Urbino Carlo Bo, Dipartimento Sci Base & Fondamenti DiSBeF, Urbino, Italy
[3] Univ Colorado, Dept Phys, Boulder, CO 80309 USA
[4] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
[5] Ohio State Univ, Sch Earth Sci, Columbus, OH 43210 USA
[6] Stanford Univ, Dept Geophys, Stanford, CA 94305 USA
[7] Univ Luxembourg, Luxembourg, Luxembourg
基金
美国国家科学基金会;
关键词
elastic uplift; GPS; ice loss; Jakobshavn; west Greenland; LAST GLACIAL MAXIMUM; SEA-LEVEL; GREENLAND; SHEET; EARTH; CONSTRAINTS; MODEL;
D O I
10.1002/jgrb.50145
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We analyze Global Positioning System (GPS) time series of relative vertical and horizontal surface displacements from 2006 to 2012 at four GPS sites located between approximate to 5 and approximate to 150km from the front of Jakobshavn Isbrae (JI) in west Greenland. Horizontal displacements during 2006-2010 at KAGA, ILUL, and QEQE, relative to the site AASI, are directed toward north-west, suggesting that the main mass loss signal is located near the frontal portion of JI. The directions of the observed displacements are supported by modeled displacements, derived from NASA's Airborne Topographic Mapper (ATM) surveys of surface elevations from 2006, 2009, and 2010. However, horizontal displacements during 2010-2012 at KAGA and ILUL are directed more towards the west suggesting a change in the spatial distribution of the ice mass loss. In addition, we observe an increase in the uplift rate during 2010-2012 as compared to 2006-2010. The sudden change in vertical and horizontal displacements is due to enhanced melt-induced ice loss in 2010 and 2012.
引用
收藏
页码:1837 / 1844
页数:8
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