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Article Dans Une Revue Annals of Glaciology Année : 1997

Ice-sheet mass balance during the last glacial maximum

Résumé

In the framework of the Paleoclimate Modelling Intercomparison Project (PMIP), simulations of the Last Glacial Maximum (LGM) have- been performed. More than 10 different atmospheric general circulation models (AGCMs) have been used with the same boundary conditions: sea-surface temperatures prescribed by CLIMAP (1981), ice-sheet reconstruction provided by Peltier (1994), change in insolation, and reduced CO2 content. One of the major questions is to investigate whether the simulations of the LGM are in equilibrium with the prescribed ice-sheet reconstruction. To answer this question, we have used two different approaches. First, we analyze the results of a sel of LGM simulations performed with different versions of the Laboratoire de Meteorolo-gie Dynamique (LMD) AGCM and study the hydrologic and snow- budgets over the Laurcntide and Fennoscandian ice sheets. Second, we use the AGCM outputs to force an ice-sheet model in order to investigate its ability to maintain the ice sheets as reconstructed by CLIMAP (1981) or Peltier (1994).
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Dates et versions

hal-03011923 , version 1 (18-12-2020)

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Gilles Ramstein, Adeline Fabre, Sophie Pinot, Catherine Ritz, Sylvie Joussaume. Ice-sheet mass balance during the last glacial maximum. Annals of Glaciology, 1997, 25, pp.145-152. ⟨10.3189/S026030550001394X⟩. ⟨hal-03011923⟩
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