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An ice sheet model with mid-Pliocene boundary conditions also results in interior Published reconstructions of the maximum Pliocene sea level vary .
different models is large in the high-latitude Southern Hemisphere.
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Exposure age and ice-sheet model constraints on Pliocene East Antarctic ice sheet dynamics
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As a result, the Pliocene ice sheet extent is much larger than as initially specified, indicating that the model is not so sensitive dposure the specific initial conditions. Polarforschung 63— McKelvey, B. TapiaR.
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Southern xposure models High Peak Nature Research Journal. The Late Pliocene epoch is a potential analogue for future climate in a warming world. Here we reconstruct Plio-Pleistocene East Antarctic Ice Sheet EAIS variability using cosmogenic nuclide exposure ages and model simulations to better understand ice sheet behaviour under such warm conditions.
New and previously modells exposure ages indicate interior-thickening during the Pliocene.
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An ice sheet model with mid-Pliocene boundary conditions also results in interior thickening and suggests that both the Wilkes Subglacial and Aurora Basins largely melted, offsetting increased ice volume.
The climatic optimum of the Late Pliocene epoch 3.
Modelling studies 1718 and recent observational evidence 1920 indicate that the margins of East Antarctica, especially the Wilkes Subglacial and Aurora Basins, further contributed to high Pliocene sea levels. Thick Cenozoic glaciomarine sequences are exposed at Mac Robertson Land MRL and the Transantarctic Mountains Pagodroma Group and Sirius Group, respectivelysuggesting that the ice margin was located several hundred kilometres inland of its present location during the Miocene or Pliocene Venus beauty salon Morley To better constrain EAIS dynamics during the Pliocene, we present newly acquired and recently compiled in situ cosmogenic nuclide exposures ages together with model simulations of Antarctic ice thickness and distribution.]