Simulations of the Northern Hemisphere through the last glacial-interglacial cycle with a vertically integrated and a three-dimensional thermomechanical ice-sheet model coupled to a climate model

Annals of Glaciology

Volumn 27, Issue , 1998, Pages 169-176

  Calov, R ^a,c   Marsiat, I ^b  

^a DARMSTADT UNIVERSITY OF TECHNOLOGY   (Germany)

^b UNIVERSITY OF READING   (United Kingdom)

^c POTSDAM INSTITUTE FOR CLIMATE IMPACT RESEARCH   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

CLIMATE MODELING; GLACIAL-INTERGLACIAL CYCLE; ICE SHEET; NORTHERN HEMISPHERE;

EID: 0032423535     PISSN: 02603055     EISSN: None     Source Type: Journal    
DOI: 10.3189/1998aog27-1-169-176     Document Type: Article

References (15)

1. Calov, R. and K. Hutter. 1996. The thermomechanical response of the Greenland ice sheet to various climate scenarios. Climate Dyn., 12, 243-260.
2. CLIMAP Project Members. 1981. Seasonal reconstructions of the Earth's surface at the last glacial maximum. Boulder, CO, Geological Society of America. (Map Chart MC-36.)
3. Deblonde, G. and W. R. Peltier. 1993. Late Pleistocene ice age scenarios based on observational evidence. J. Climate, 6(4), 709-727.
4. Gallće, H., J. P. van Ypersele, T. Fichefet, C. Tricot and A. Berger. 1991. Simulation of the last glacial cycle by a coupled, sectorially averaged climate-ice sheet model. 1. The climate model. J. Geophys. Res., 96(D7), 13,139-13,161.
5. Greve, R. 1997. Application of a polythermal three-dimensional ice sheet model to the Greenland ice sheet: response to steady-state and transient climate scenarios. J. Climate, 10(5), 901-918.
6. Huybrechts, P. and J. Oerlemans. 1988. Evolution of the East Antarctic ice sheet: a numerical study of thermo-mechanical response patterns with changing climate. Ann. Glaciol., 11, 52-59.
7. Huybrechts, P. and S. T'siobbel. 1997. A three-dimensional climate-ice-sheet model applied to the Last Glacial Maximum. Ann. Glaciol., 25, 333-339.
8. Marsiat, I. 1994. Simulation of the Northern Hemisphere continental ice sheets over the last glacial-interglacial cycle: experiments with a latitude-longitude vertically integrated ice sheet model coupled to a zonally averaged climate model. Paleoclimates, 1, 59-98.
9. Paterson, W. S. B. 1981. The physics of glaciers. Second edition. Oxford, etc., Pergamon Press.
10. Peltier, W. R. and S. Marshall. 1995. Coupled energy-balance/ice-sheet model simulations of the glacial cycle: a possible connection between terminations and terrigenous dust. J. Geophys. Res., 100(D7), 14,269-14,289.
11. Ritz, C., A. Fabre and A. Letréguilly. 1997. Sensitivity of a Greenland ice sheet model to ice flow and ablation parameters: consequences for the evolution through the Last Glacial cycle. Climate Dyn., 13, 11-24.
12. Sellers, W. D. 1983. A quasi-three-dimensional climate model. J. Climate Appl. Meteorol., 22, 1552-1574.
13. Tarasov, L. and W. R. Peltier. 1997. Terminating the 100 kyr ice age cycle. J. Geophys. Res., 102(D18), 21,665-21,693.
14. Tushingham, A. M. and W. R. Peltier. 1991. Ice-3G: a new global model of late Pleistocene deglaciation based upon geophysical predictions of post-glacial relative sea level change. J. Geophys. Res., 96(B3), 4497-4523.
15. Weertman, J. 1964. The theory of glacier sliding. J. Glaciol., 5(39), 287-303.