Synthesizing multiple remote-sensing techniques for subglacial hydrologic mapping: application to a lake system beneath MacAyeal Ice Stream, West Antarctica

被引:43
作者
Fricker, Helen Amanda [1 ]
Scambos, Ted [2 ]
Carter, Sasha [1 ]
Davis, Curt [3 ]
Haran, Terry [2 ]
Joughin, Ian [4 ]
机构
[1] Univ Calif San Diego, Scripps Inst Oceanog, Inst Geophys & Planetary Phys, La Jolla, CA 92093 USA
[2] Univ Colorado, CIRES, Natl Snow & Ice Data Ctr, Boulder, CO 80309 USA
[3] Univ Missouri, Columbia, MO 65211 USA
[4] Univ Washington, Appl Phys Lab, Polar Sci Ctr, Seattle, WA 98105 USA
关键词
LASER ALTIMETRY; GROUNDING ZONE; RADAR; IDENTIFICATION; INVENTORY; FLOODS; MODEL; SHELF;
D O I
10.3189/002214310791968557
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
We present an analysis of the active hydrologic system of MacAyeal Ice Stream (MacIS), West Antarctica, from a synthesis of multiple remote-sensing techniques: satellite laser altimetry; satellite image differencing; and hydrologic potential mapping (using a satellite-derived DEM and a bedrock DEM from airborne radio-echo sounding). Combining these techniques augments the information provided by each one individually, and allows us to develop a protocol for studying subglacial hydrologic systems in a holistic manner. Our study reveals five large active subglacial lakes under MacIS, the largest of which undergoes volume changes of at least 1.0 km(3). We discuss the hydrologic properties of this system and present evidence for links between the lakes. At least three of the lakes are co-located with sticky spots, i.e. regions of high local basal shear stress. We also find evidence for surface elevation changes due to ice-dynamic effects (not just water movement) caused by changes in basal resistance. Lastly, we show that satellite radar altimetry is of limited use for monitoring lake activity on fast-flowing ice streams with surfaces that undulate on similar to 10 km length scales.
引用
收藏
页码:187 / 199
页数:13
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