Englacial latent-heat transfer has limited influence on seaward ice flux in western Greenland

Surface meltwater can refreeze within firn layers and crevasses to warm ice through latent-heat transfer on decadal to millennial timescales. Earlier work posited that the consequent softening of the ice might accelerate ice flow, potentially increasing ice-sheet mass loss. Here, we calculate the ef...

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Bibliographic Details
Main Authors: Poinar, Kristin, Joughin, Ian, Lenaerts, Jan T.M., Van Den Broeke, Michiel R.
Other Authors: Sub Dynamics Meteorology, Marine and Atmospheric Research
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Online Access:https://dspace.library.uu.nl/handle/1874/350702