Exposure age and ice-sheet model constraints on Pliocene East Antarctic ice sheet dynamics

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. Ne...

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Bibliographic Details
Published in:Nature Communications
Main Authors: Yamane, Masako, Yokoyama, Yusuke, Abe-Ouchi, Ayako, Obrochta, Stephen, Saito, Fuyuki, Moriwaki, Kiichi, Matsuzaki, Hiroyuki
Format: Text
Language:English
Published: Nature Pub. Group 2015
Subjects:
Article
Antarctic
East Antarctic Ice Sheet
Greenland
West Antarctica
Antarc*
Antarctica
Ice Sheet
Sea ice
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4421805/
http://www.ncbi.nlm.nih.gov/pubmed/25908601
https://doi.org/10.1038/ncomms8016
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Summary: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 published exposure ages indicate interior-thickening during the Pliocene. 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. Considering contributions from West Antarctica and Greenland, this is consistent with the most recent IPCC AR5 estimate, which indicates that the Pliocene sea level likely did not exceed +20 m on Milankovitch timescales. The inception of colder climate since ∼3 Myr has increased the sea ice cover and inhibited active moisture transport to Antarctica, resulting in reduced ice sheet thickness, at least in coastal areas.

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