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Antarctic climate and ice-sheet configuration during the early Pliocene interglacial at 4.23 Ma

Antarctic climate and ice-sheet configuration during the early Pliocene interglacial at 4.23 Ma
Antarctic climate and ice-sheet configuration during the early Pliocene interglacial at 4.23 Ma
The geometry of Antarctic ice sheets during warm periods of the geological past is difficult to determine from geological evidence, but is important to know because such reconstructions enable a more complete understanding of how the ice-sheet system responds to changes in climate. Here we investigate how Antarctica evolved under orbital and greenhouse gas conditions representative of an interglacial in the early Pliocene at 4.23 Ma, when Southern Hemisphere insolation reached a maximum. Using offline-coupled climate and ice-sheet models, together with a new synthesis of high-latitude palaeoenvironmental proxy data to define a likely climate envelope, we simulate a range of ice-sheet geometries and calculate their likely contribution to sea level. In addition, we use these simulations to investigate the processes by which the West and East Antarctic ice sheets respond to environmental forcings and the timescales over which these behaviours manifest. We conclude that the Antarctic ice sheet contributed 8.6 ± 2.8 m to global sea level at this time, under an atmospheric CO2 concentration identical to present (400 ppm). Warmer-than-present ocean temperatures led to the collapse of West Antarctica over centuries, whereas higher air temperatures initiated surface melting in parts of East Antarctica that over one to two millennia led to lowering of the ice-sheet surface, flotation of grounded margins in some areas, and retreat of the ice sheet into the Wilkes Subglacial Basin. The results show that regional variations in climate, ice-sheet geometry, and topography produce long-term sea-level contributions that are non-linear with respect to the applied forcings, and which under certain conditions exhibit threshold behaviour associated with behavioural tipping points.
1814-9324
959-975
Golledge, Nicholas R.
6e5f88b4-366b-49f9-81fe-3354a1bd7d88
Thomas, Zoë A.
4b512d3a-3478-4270-9fdd-61256aa640d3
Levy, Richard H.
4e173f48-fde8-44ec-b900-c3e143825de9
Gasson, Edward G.W.
075df12d-7495-4f5a-bd25-3cdd9797d560
Naish, Timothy R.
99010d96-f939-429b-a8c0-6fe25fb97040
McKay, Robert M.
11eaad44-da67-46e3-9b47-d9464a4ae0a1
Kowalewski, Douglas E.
470ce496-97ae-461f-8665-961dc9c25a21
Fogwill, Christopher J.
3bad6ae9-5a6d-467e-b523-9d5ed0147455
et al.
Golledge, Nicholas R.
6e5f88b4-366b-49f9-81fe-3354a1bd7d88
Thomas, Zoë A.
4b512d3a-3478-4270-9fdd-61256aa640d3
Levy, Richard H.
4e173f48-fde8-44ec-b900-c3e143825de9
Gasson, Edward G.W.
075df12d-7495-4f5a-bd25-3cdd9797d560
Naish, Timothy R.
99010d96-f939-429b-a8c0-6fe25fb97040
McKay, Robert M.
11eaad44-da67-46e3-9b47-d9464a4ae0a1
Kowalewski, Douglas E.
470ce496-97ae-461f-8665-961dc9c25a21
Fogwill, Christopher J.
3bad6ae9-5a6d-467e-b523-9d5ed0147455

Golledge, Nicholas R., Thomas, Zoë A., Levy, Richard H. and Gasson, Edward G.W. , et al. (2017) Antarctic climate and ice-sheet configuration during the early Pliocene interglacial at 4.23 Ma. Climate of the Past, 13 (7), 959-975. (doi:10.5194/cp-13-959-2017).

Record type: Article

Abstract

The geometry of Antarctic ice sheets during warm periods of the geological past is difficult to determine from geological evidence, but is important to know because such reconstructions enable a more complete understanding of how the ice-sheet system responds to changes in climate. Here we investigate how Antarctica evolved under orbital and greenhouse gas conditions representative of an interglacial in the early Pliocene at 4.23 Ma, when Southern Hemisphere insolation reached a maximum. Using offline-coupled climate and ice-sheet models, together with a new synthesis of high-latitude palaeoenvironmental proxy data to define a likely climate envelope, we simulate a range of ice-sheet geometries and calculate their likely contribution to sea level. In addition, we use these simulations to investigate the processes by which the West and East Antarctic ice sheets respond to environmental forcings and the timescales over which these behaviours manifest. We conclude that the Antarctic ice sheet contributed 8.6 ± 2.8 m to global sea level at this time, under an atmospheric CO2 concentration identical to present (400 ppm). Warmer-than-present ocean temperatures led to the collapse of West Antarctica over centuries, whereas higher air temperatures initiated surface melting in parts of East Antarctica that over one to two millennia led to lowering of the ice-sheet surface, flotation of grounded margins in some areas, and retreat of the ice sheet into the Wilkes Subglacial Basin. The results show that regional variations in climate, ice-sheet geometry, and topography produce long-term sea-level contributions that are non-linear with respect to the applied forcings, and which under certain conditions exhibit threshold behaviour associated with behavioural tipping points.

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Published date: 27 July 2017
Additional Information: Funding Information: We are grateful to the two anonymous reviewers for their comments on a previous version of this manuscript. This work was funded by contract VUW1203 of the Royal Society of New Zealand's Marsden Fund, with support from the Antarctic Research Centre, Victoria University of Wellington, ANDRILL, GNS Science, NSF Polar Programs grants ANT-1043712 and PLR-1245899, and the Australian Research Council (ARC) including a Laureate Fellowship (FL100100195) supporting Zoë A. Thomas. We are very grateful to PISM developers for their continued support. PISM is supported by NASA grants NNX13AM16G and NNX13AK27G. Publisher Copyright: © Author(s) 2017.

Identifiers

Local EPrints ID: 476044
URI: http://eprints.soton.ac.uk/id/eprint/476044
ISSN: 1814-9324
PURE UUID: 7ddecf9a-e195-40c1-bd1b-a6e2a01275c0
ORCID for Zoë A. Thomas: ORCID iD orcid.org/0000-0002-2323-4366

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Date deposited: 04 Apr 2023 17:00
Last modified: 18 Mar 2024 04:10

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Contributors

Author: Nicholas R. Golledge
Author: Zoë A. Thomas ORCID iD
Author: Richard H. Levy
Author: Edward G.W. Gasson
Author: Timothy R. Naish
Author: Robert M. McKay
Author: Douglas E. Kowalewski
Author: Christopher J. Fogwill
Corporate Author: et al.

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