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...
Published in: | Journal of Glaciology |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
2016
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Subjects: | |
Online Access: | http://dx.doi.org/10.1017/jog.2016.103 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143016001039 |