Net effect of ice-sheet-atmosphere interactions reduces simulated transient Miocene Antarctic ice-sheet variability
Benthic δ18O levels vary strongly during the warmer-than-modern early and mid-Miocene (23 to 14 Myr ago), suggesting a dynamic Antarctic ice sheet (AIS). So far, however, realistic simulations of the Miocene AIS have been limited to equilibrium states under different CO2 levels and orbital settings....
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus GmbH
2022
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| Subjects: | |
| Online Access: | View Fulltext in Publisher |