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Simulating arctic climate warmth and icefield retreat in the last interglaciation

Simulating arctic climate warmth and icefield retreat in the last interglaciation
Simulating arctic climate warmth and icefield retreat in the last interglaciation
In the future, Arctic warming and the melting of polar glaciers will be considerable, but the magnitude of both is uncertain. We used a global climate model, a dynamic ice sheet model, and paleoclimatic data to evaluate Northern Hemisphere high-latitude warming and its impact on Arctic icefields during the Last Interglaciation. Our simulated climate matches paleoclimatic observations of past warming, and the combination of physically based climate and ice-sheet modeling with icecore constraints indicate that the Greenland Ice Sheet and other circum-Arctic ice fields likely contributed 2.2 to 3.4 meters of sea-level rise during the Last Interglaciation.
0036-8075
1751-1753
Otto-Bliesner, Beth L.
8c08adba-a0d4-4d83-8d36-e4bb9f099b79
Marsha, Shawn J.
cbb6ccf5-cea5-42cd-93b0-d42ac5ec6415
Overpeck, Jonathan T.
6110c685-7710-4460-b41c-e07d5e0d40ba
Miller, Gifford H.
93b3a78d-0515-44d9-a192-d11d0bf420fc
Hu, Aixue X.
b1f153e2-c617-4674-8565-c8ba186f2fb6
Edwards, M.E
4b6a3389-f3a4-4933-b8fd-acdfef72200e
CAPE Last Interglacial Project members
Otto-Bliesner, Beth L.
8c08adba-a0d4-4d83-8d36-e4bb9f099b79
Marsha, Shawn J.
cbb6ccf5-cea5-42cd-93b0-d42ac5ec6415
Overpeck, Jonathan T.
6110c685-7710-4460-b41c-e07d5e0d40ba
Miller, Gifford H.
93b3a78d-0515-44d9-a192-d11d0bf420fc
Hu, Aixue X.
b1f153e2-c617-4674-8565-c8ba186f2fb6
Edwards, M.E
4b6a3389-f3a4-4933-b8fd-acdfef72200e

Otto-Bliesner, Beth L., Marsha, Shawn J., Overpeck, Jonathan T., Miller, Gifford H., Hu, Aixue X. and Edwards, M.E , CAPE Last Interglacial Project members (2006) Simulating arctic climate warmth and icefield retreat in the last interglaciation. Science, 311 (5768), 1751-1753. (doi:10.1126/science.1120808).

Record type: Article

Abstract

In the future, Arctic warming and the melting of polar glaciers will be considerable, but the magnitude of both is uncertain. We used a global climate model, a dynamic ice sheet model, and paleoclimatic data to evaluate Northern Hemisphere high-latitude warming and its impact on Arctic icefields during the Last Interglaciation. Our simulated climate matches paleoclimatic observations of past warming, and the combination of physically based climate and ice-sheet modeling with icecore constraints indicate that the Greenland Ice Sheet and other circum-Arctic ice fields likely contributed 2.2 to 3.4 meters of sea-level rise during the Last Interglaciation.

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More information

Published date: 24 March 2006

Identifiers

Local EPrints ID: 55288
URI: http://eprints.soton.ac.uk/id/eprint/55288
ISSN: 0036-8075
PURE UUID: 9a5e7311-543c-474f-8e3f-bcf082c0c90b
ORCID for M.E Edwards: ORCID iD orcid.org/0000-0002-3490-6682

Catalogue record

Date deposited: 01 Aug 2008
Last modified: 16 Mar 2024 03:27

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Contributors

Author: Beth L. Otto-Bliesner
Author: Shawn J. Marsha
Author: Jonathan T. Overpeck
Author: Gifford H. Miller
Author: Aixue X. Hu
Author: M.E Edwards ORCID iD
Corporate Author: CAPE Last Interglacial Project members

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