期刊
JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE
卷 122, 期 12, 页码 2488-2505出版社
AMER GEOPHYSICAL UNION
DOI: 10.1002/2016JF004187
关键词
Arctic glaciology; ice velocity; crevasses; glacier flow; glacial hydrology
资金
- National Aeronautics and Space Administration [NNX15AH84G, NNX16AJ88G]
The impact of meltwater injection into the shear margins of Jakobshavn Isbrae via drainage from water-filled crevasses on ice flow is examined. We use Landsat-8 Operational Land Imager panchromatic, high-resolution imagery to monitor the spatiotemporal variability of seven water-filled crevasse ponds during the summers of 2013 to 2015. The timing of drainage from water-filled crevasses coincides with an increase of 2 to 20% in measured ice velocity beyond Jakobshavn Isbrae shear margins, which we define as extramarginal ice velocity. Some water-filled crevasse groups demonstrate multiple drainage events within a single melt season. Numerical simulations show that hydrologic shear weakening due to water-filled crevasse drainage can accelerate extramarginal flow by as much as similar to 35% within 10km of the margins and enhance mass flux through the shear margins by 12%. This work demonstrates a novel mechanism through which surface melt can influence regional ice flow.
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