Crynodeb
The Greenland Ice Sheet is thinning at an accelerating pace and the ice sheet’s
contribution to sea-level rise has doubled in less than a decade. New data show
rapid and widespread changes in the behaviour of the ice sheet, particularly
along the coastal margin. These changes coincide with a decade of sustained
Arctic warming of up to 3 °C. Decay of the Greenland Ice Sheet in response to
global warming will not only be governed by increased surface melting during
longer and warmer summers but also by a speed-up of coastal glaciers that
drain the interior ice sheet. A precise estimate of sea-level rise in the twentyfirst
century relies on improved theoretical treatment of these glaciers in computer models
Iaith wreiddiol | Saesneg |
---|---|
Tudalennau (o-i) | 98-103 |
Nifer y tudalennau | 6 |
Cyfnodolyn | Geology Today |
Cyfrol | 22 |
Rhif cyhoeddi | 3 |
Dynodwyr Gwrthrych Digidol (DOIs) | |
Statws | Cyhoeddwyd - Mai 2006 |