CORDIS Project
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This project re-evaluates the role of surface meltwater in the dynamics of the Greenland Ice Sheet. It aims to understand how glacier morphology influences ice loss and predict future sea-level changes based on these insights.
Over just three decades, the Greenland Ice Sheet contribution to sea-level rise has grown six-fold.
Increased basal slipperiness from increased surface melt was initially proposed as a key mechanism reinforcing ice loss, but a wealth of studies deconstructed this idea, leading the Intergovernmental Panel on Climate Change (IPCC) to conclude that increased surface melt “has not led to sustained increases in glacier flux”.
Last year, however, my group re-established meltwater as a primary mechanis…
CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE CNRS
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