The role of history and strength of the oceanic forcing in sea level projections from Antarctica with the Parallel Ice Sheet Model
<p>Mass loss from the Antarctic Ice Sheet constitutes the largest uncertainty in projections of future sea level rise. Ocean-driven melting underneath the floating ice shelves and subsequent acceleration of the inland ice streams are the major reasons for currently observed mass loss from Anta...
| Main Authors: | , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2020-09-01
|
| Series: | The Cryosphere |
| Online Access: | https://tc.copernicus.org/articles/14/3097/2020/tc-14-3097-2020.pdf |