Abstract
In recent decades, Greenland's peripheral glaciers have experienced
large-scale mass loss, resulting in a substantial contribution to sea
level rise. While their total area of Greenland ice cover is relatively
small (4%), their mass loss is disproportionally large compared to the
Greenland ice sheet. Satellite altimetry from Ice, Cloud, and land
Elevation Satellite (ICESat) and ICESat-2 shows that mass loss from
Greenland's peripheral glaciers increased from 27.2 ± 6.2 Gt/yr
(February 2003–October 2009) to 42.3 ± 6.2 Gt/yr (October 2018–December
2021). These relatively small glaciers now constitute 11 ± 2% of
Greenland's ice loss and contribute to global sea level rise. In the
period October 2018–December 2021, mass loss increased by a factor of
four for peripheral glaciers in North Greenland. While peripheral
glacier mass loss is widespread, we also observe a complex regional
pattern where increases in precipitation at high altitudes have
partially counteracted increases in melt at low altitude.
| Original language | English |
|---|---|
| Article number | e2022GL098915 |
| Journal | Geophysical Research Letters |
| Volume | 49 |
| Issue number | 12 |
| Number of pages | 8 |
| ISSN | 0094-8276 |
| DOIs | |
| Publication status | Published - 2022 |
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