Abstract
Sedimentation filling space beneath ice shelves helps to stabilize ice sheets against grounding-line retreat in response to a rise in relative sea level of at least several meters. Recent Antarctic changes thus cannot be attributed to sea-level rise, strengthening earlier interpretations that warming has driven ice-sheet mass loss. Large sea-level rise, such as the ≈100-meter rise at the end of the last ice age, may overwhelm the stabilizing feedback from sedimentation, but smaller sea-level changes are unlikely to have synchronized the behavior of ice sheets in the past.
Original language | English (US) |
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Pages (from-to) | 1838-1841 |
Number of pages | 4 |
Journal | Science |
Volume | 315 |
Issue number | 5820 |
DOIs | |
State | Published - Mar 30 2007 |
All Science Journal Classification (ASJC) codes
- General