Resumé
Accurate projections of the mass loss from the Greenland Ice Sheet (GrIS) require a complete understanding of the ice-dynamic response to climate forcings on seasonal and interannual timescales and would greatly benefit from more observational evidence. Here, we analyze a 5-year, high-resolution data set of ice velocities of the GrIS using K-means, an unsupervised clustering algorithm, to identify ice-sheet wide characteristic seasonal flow patterns. We include all areas flowing >0.3 m/d and obtain an ice-sheet wide overview of the seasonality and the interannual variability. It shows both a spatial and interannual variability in seasonal flow patterns, both along individual glaciers and between glaciers. We compare with runoff from a regional climate model and infer that the ice-sheet wide patterns are linked to the availability of water penetrating to the base of the ice.
| Originalsprog | Engelsk |
|---|---|
| Artikelnummer | e2022GL100343 |
| Antal sider | 10 |
| Tidsskrift | Geophysical Research Letters |
| Vol/bind | 49 |
| Udgave nummer | 24 |
| DOI | |
| Status | Udgivet - 28 dec. 2022 |
FN’s Verdensmål
Dette resultat bidrager til følgende verdensmål
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Verdensmål 13 Klimaindsats
Programområde
- Programområde 5: Natur og klima
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