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Rapid ice flow rearrangement induced by subglacial drainage in West Antarctica
Author(s) -
Elsworth Cooper W.,
Suckale Jenny
Publication year - 2016
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2016gl070430
Subject(s) - meltwater , geology , ice stream , streams , ice divide , ice sheet , antarctic ice sheet , geomorphology , ice shelf , antarctic sea ice , drainage , lead (geology) , cryosphere , climatology , sea ice , glacier , computer science , biology , computer network , ecology
Abstract Ice streams are corridors of rapid ice flow draining the ice sheets. They can exhibit astonishing spatial variability on annual to centennial time scales. We propose that changes in the subglacial drainage of meltwater could induce these sudden rearrangements of ice streams. We develop a two‐dimensional, thermomechanical model representing an ice stream cross section and couple it to a plastically deforming bed with spatially variable meltwater influx. We find that where ice flows over deformable sediments and lacks significant topographic control, the efficiency of subglacial water drainage exerts direct control on the velocity, location, and width of ice streams. This implies that meltwater percolation at the meter scale could have a significant effect on the short‐term variability in ice loss from a continental‐scale ice sheet. We verify our model against previous analytical results and validate it against surface observations from the Siple Coast of West Antarctica.