Affiliation:
1. School of Geosciences University of Edinburgh Edinburgh UK
2. Department of Geography University of Sheffield Sheffield UK
3. Department of Geosciences University of Fribourg Fribourg Switzerland
4. NASA Goddard Institute for Space Studies New York NY USA
5. Autonomic Integra LLC New York NY USA
Abstract
AbstractExtreme melt and rainfall events can induce temporary acceleration of Greenland Ice Sheet motion, leading to increased advection of ice to lower elevations where melt rates are higher. In a warmer climate, these events are likely to become more frequent. In September 2022, seasonally unprecedented air temperatures caused multiple melt events over the Greenland Ice Sheet, generating the highest melt rates of the year. The scale and timing of the largest event overwhelmed the subglacial drainage system, enhancing basal sliding and increasing ice velocities by up to ∼240% relative to pre‐event velocities. However, ice motion returned rapidly to pre‐event levels, and the speed‐ups caused a regional increase in annual ice discharge of only ∼2% compared to when the effects of the speed‐ups were excluded. Therefore, although late melt‐season events are forecast to become more frequent and drive significant runoff, their impact on net mass loss via ice discharge is minimal.
Funder
Natural Environment Research Council
European Research Council
Swiss Polar Institute
Publisher
American Geophysical Union (AGU)
Cited by
1 articles.
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