|Ice sheet and solid earth influences on far-field sea-level histories|
Bassett, S.E.; Milne, G.A.; Mitrovica, J.X.; Clark, P.U. (2005). Ice sheet and solid earth influences on far-field sea-level histories. Science (Wash.) 309(5736): 925-928
In: Science (Washington). American Association for the Advancement of Science: New York, N.Y. ISSN 0036-8075, more
|Also published as |
- Bassett, S.E.; Milne, G.A.; Mitrovica, J.X.; Clark, P.U. (2005). Ice sheet and solid earth influences on far-field sea-level histories. Science (Wash.) 308(5730): 10.1126/science.1111575, more
Climatic changes; Glaciation; Sea level; Marine
|Authors|| || Top |
- Bassett, S.E.
- Milne, G.A.
- Mitrovica, J.X.
- Clark, P.U.
Previous predictions of sea-level change subsequent to the last glacial maximum show significant, systematic discrepancies between observations at Tahiti, Huon Peninsula, and Sunda Shelf during Lateglacial time (~14,000 to 9000 calibrated years before the present). We demonstrate that a model of glacial isostatic adjustment characterized by both a high-viscosity lower mantle (4 x 10²² Pa s) and a large contribution from the Antarctic ice sheet to meltwater pulse IA (~15-meters eustatic equivalent) resolves these discrepancies. This result supports arguments that an early and rapid Antarctic deglaciation contributed to a sequence of climatic events that ended the most recent glacial period of the current ice age.