A new model of dry firn-densification constrained by continuous strain measurements near South Pole
Converting measurements of ice-sheet surface elevation change to mass change requires measurements of accumulation and knowledge of the evolution of the density profile in the firn. Most firn-densification models are tuned using measured depth–density profiles, a method which is based on an assumpti...
Main Authors: | , , , , , |
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Format: | Article |
Language: | English |
Published: |
Cambridge University Press
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Series: | Journal of Glaciology |
Subjects: | |
Online Access: | https://www.cambridge.org/core/product/identifier/S0022143023000874/type/journal_article |