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

ABSTRACT 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 calcula...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: POINAR, KRISTIN, JOUGHIN, IAN, LENAERTS, JAN T. M., VAN DEN BROEKE, MICHIEL R.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2016
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2016.103
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143016001039