A comparison of different ways of dealing with isostasy: examples from modeling the Antarctic ice sheet during the last glacial cycle
The bedrock isostatic response exerts a strong control on ice sheet dynamics and is therefore always taken into account in ice sheet models. This paperreviews the various methods normally used in the ice-sheet modeling community to deal with the bedrock response and compares these with a moresophist...
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ftawi:oai:epic.awi.de:2128 2023-09-05T13:12:05+02:00 A comparison of different ways of dealing with isostasy: examples from modeling the Antarctic ice sheet during the last glacial cycle Le Meur, E. Huybrechts, Philippe 1996 application/pdf https://epic.awi.de/id/eprint/2128/ https://epic.awi.de/id/eprint/2128/1/Meu1995a.pdf https://hdl.handle.net/10013/epic.12717 https://hdl.handle.net/10013/epic.12717.d001 unknown https://epic.awi.de/id/eprint/2128/1/Meu1995a.pdf https://hdl.handle.net/10013/epic.12717.d001 Le Meur, E. and Huybrechts, P. (1996) A comparison of different ways of dealing with isostasy: examples from modeling the Antarctic ice sheet during the last glacial cycle , Annals of Glaciology, 23 , pp. 309-317 . hdl:10013/epic.12717 EPIC3Annals of Glaciology, 23, pp. 309-317 Article isiRev 1996 ftawi 2023-08-22T19:43:08Z The bedrock isostatic response exerts a strong control on ice sheet dynamics and is therefore always taken into account in ice sheet models. This paperreviews the various methods normally used in the ice-sheet modeling community to deal with the bedrock response and compares these with a moresophisticated full Earth model. Each of these bedrock treatments, five in total, are coupled with a three-dimensional thermomechanical ice sheet model underthe same forcing conditions to simulate the Antarctic ice sheet during the last glacial cycle. The outputs of the simulations are compared on the basis of thetime-dependent behavior for the total ice volume and the mean bedrock elevation during the cycle, and of the present rate of uplift over Antarctica. Thiscomparison confirms the necessity of accounting for the elastic bending of the lithosphere in order to yield realistic bedrock patterns. It furthermoredemonstrates the deficiencies inherent to the diffusion equation in modeling the complex deformation within the mantle. Nevertheless, when characteristicparameters are varied within their range of uncertainty, differences within one single method are often of the same order as those between the variousmethods. This overview finally tries to point out the main advantages and drawbacks of each of these methods and to determine which one is mostappropriate depending on the specific modeling requirements. Article in Journal/Newspaper Annals of Glaciology Antarc* Antarctic Antarctica Ice Sheet Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Antarctic The Antarctic |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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description |
The bedrock isostatic response exerts a strong control on ice sheet dynamics and is therefore always taken into account in ice sheet models. This paperreviews the various methods normally used in the ice-sheet modeling community to deal with the bedrock response and compares these with a moresophisticated full Earth model. Each of these bedrock treatments, five in total, are coupled with a three-dimensional thermomechanical ice sheet model underthe same forcing conditions to simulate the Antarctic ice sheet during the last glacial cycle. The outputs of the simulations are compared on the basis of thetime-dependent behavior for the total ice volume and the mean bedrock elevation during the cycle, and of the present rate of uplift over Antarctica. Thiscomparison confirms the necessity of accounting for the elastic bending of the lithosphere in order to yield realistic bedrock patterns. It furthermoredemonstrates the deficiencies inherent to the diffusion equation in modeling the complex deformation within the mantle. Nevertheless, when characteristicparameters are varied within their range of uncertainty, differences within one single method are often of the same order as those between the variousmethods. This overview finally tries to point out the main advantages and drawbacks of each of these methods and to determine which one is mostappropriate depending on the specific modeling requirements. |
format |
Article in Journal/Newspaper |
author |
Le Meur, E. Huybrechts, Philippe |
spellingShingle |
Le Meur, E. Huybrechts, Philippe A comparison of different ways of dealing with isostasy: examples from modeling the Antarctic ice sheet during the last glacial cycle |
author_facet |
Le Meur, E. Huybrechts, Philippe |
author_sort |
Le Meur, E. |
title |
A comparison of different ways of dealing with isostasy: examples from modeling the Antarctic ice sheet during the last glacial cycle |
title_short |
A comparison of different ways of dealing with isostasy: examples from modeling the Antarctic ice sheet during the last glacial cycle |
title_full |
A comparison of different ways of dealing with isostasy: examples from modeling the Antarctic ice sheet during the last glacial cycle |
title_fullStr |
A comparison of different ways of dealing with isostasy: examples from modeling the Antarctic ice sheet during the last glacial cycle |
title_full_unstemmed |
A comparison of different ways of dealing with isostasy: examples from modeling the Antarctic ice sheet during the last glacial cycle |
title_sort |
comparison of different ways of dealing with isostasy: examples from modeling the antarctic ice sheet during the last glacial cycle |
publishDate |
1996 |
url |
https://epic.awi.de/id/eprint/2128/ https://epic.awi.de/id/eprint/2128/1/Meu1995a.pdf https://hdl.handle.net/10013/epic.12717 https://hdl.handle.net/10013/epic.12717.d001 |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Annals of Glaciology Antarc* Antarctic Antarctica Ice Sheet |
genre_facet |
Annals of Glaciology Antarc* Antarctic Antarctica Ice Sheet |
op_source |
EPIC3Annals of Glaciology, 23, pp. 309-317 |
op_relation |
https://epic.awi.de/id/eprint/2128/1/Meu1995a.pdf https://hdl.handle.net/10013/epic.12717.d001 Le Meur, E. and Huybrechts, P. (1996) A comparison of different ways of dealing with isostasy: examples from modeling the Antarctic ice sheet during the last glacial cycle , Annals of Glaciology, 23 , pp. 309-317 . hdl:10013/epic.12717 |
_version_ |
1776198861124009984 |