Grounding line variability and subglacial lake drainage on Pine Island Glacier, Antarctica
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Title
Grounding line variability and subglacial lake drainage on Pine Island Glacier, Antarctica
Authors
Keywords
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Journal
GEOPHYSICAL RESEARCH LETTERS
Volume 43, Issue 17, Pages 9093-9102
Publisher
American Geophysical Union (AGU)
Online
2016-08-18
DOI
10.1002/2016gl070259
References
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Related references
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- Widespread, rapid grounding line retreat of Pine Island, Thwaites, Smith, and Kohler glaciers, West Antarctica, from 1992 to 2011
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- Retreat of Pine Island Glacier controlled by marine ice-sheet instability
- (2014) L. Favier et al. Nature Climate Change
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- Channelized Ice Melting in the Ocean Boundary Layer Beneath Pine Island Glacier, Antarctica
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- The supply of subglacial meltwater to the grounding line of the Siple Coast, West Antarctica
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- Antarctic grounding line mapping from differential satellite radar interferometry
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- Variability of basal melt beneath the Pine Island Glacier ice shelf, West Antarctica
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- Convection-Driven Melting near the Grounding Lines of Ice Shelves and Tidewater Glaciers
- (2011) Adrian Jenkins JOURNAL OF PHYSICAL OCEANOGRAPHY
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- SPIRIT. SPOT 5 stereoscopic survey of Polar Ice: Reference Images and Topographies during the fourth International Polar Year (2007–2009)
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- Increased flow speed on a large East Antarctic outlet glacier caused by subglacial floods
- (2008) Leigh A. Stearns et al. Nature Geoscience
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