Localized plumes drive front-wide ocean melting of a Greenlandic tidewater glacier
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Recent acceleration of Greenland's ocean-terminating glaciers has substantially amplified the ice sheet's contribution to global sea level. Increased oceanic melting of these tidewater glaciers is widely cited as the likely trigger, and is thought to be highest within vigorous plumes driven by freshwater drainage from beneath glaciers. Yet melting of the larger part of calving fronts outside of plumes remains largely unstudied. Here we combine ocean observations collected within 100 m of a tidewater glacier with a numerical model to show that unlike previously assumed, plumes drive an energetic fjord-wide circulation which enhances melting along the entire calving front. Compared to estimates of melting within plumes alone, this fjord-wide circulation effectively doubles the glacier-wide melt rate, and through shaping the calving front has a potential dynamic impact on calving. Our results suggest that melting driven by fjord-scale circulation should be considered in process-based projections of Greenland's sea level contribution.
Slater , D A , Straneo , F , Das , S B , Richards , C G , Wagner , T J W & Nienow , P W 2018 , ' Localized plumes drive front-wide ocean melting of a Greenlandic tidewater glacier ' , Geophysical Research Letters , vol. 45 , no. 22 , pp. 12,350-12,358 . https://doi.org/10.1029/2018GL080763
Geophysical Research Letters
Copyright © 2018. American Geophysical Union. All Rights Reserved. This work has been made available online in accordance with publisher policies or with permission. Permission for further reuse of this content should be sought from the publisher or the rights holder. This is the final published version of the work, which was originally published at https://doi.org/10.1029/2018GL080763
DescriptionSupport was provided by the National Science Foundation (NSF) through PLR-1418256 and PLR-1744835, and through Woods Hole Oceanographic Institution (WHOI) Ocean and Climate Change Institute (OCCI) and the Clark Foundation. This work was also supported by a UK Natural Environmental Research Council (NERC) PhD studentship (NE/L501566/1) and Scottish Alliance for Geoscience, Environment & Society (SAGES) early career research exchange funding to D. A. S.
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