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Calving rates at tidewater glaciers vary strongly with ocean temperature

Adrian Luckman (), Douglas I. Benn, Finlo Cottier, Suzanne Bevan, Frank Nilsen and Mark Inall
Additional contact information
Adrian Luckman: College of Science, Swansea University
Douglas I. Benn: University Centre in Svalbard
Finlo Cottier: Scottish Association for Marine Science
Suzanne Bevan: College of Science, Swansea University
Frank Nilsen: University Centre in Svalbard
Mark Inall: Scottish Association for Marine Science

Nature Communications, 2015, vol. 6, issue 1, 1-7

Abstract: Abstract Rates of ice mass loss at the calving margins of tidewater glaciers (frontal ablation rates) are a key uncertainty in sea level rise projections. Measurements are difficult because mass lost is replaced by ice flow at variable rates, and frontal ablation incorporates sub-aerial calving, and submarine melt and calving. Here we derive frontal ablation rates for three dynamically contrasting glaciers in Svalbard from an unusually dense series of satellite images. We combine ocean data, ice-front position and terminus velocity to investigate controls on frontal ablation. We find that frontal ablation is not dependent on ice dynamics, nor reduced by glacier surface freeze-up, but varies strongly with sub-surface water temperature. We conclude that calving proceeds by melt undercutting and ice-front collapse, a process that may dominate frontal ablation where submarine melt can outpace ice flow. Our findings illustrate the potential for deriving simple models of tidewater glacier response to oceanographic forcing.

Date: 2015
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DOI: 10.1038/ncomms9566

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