A model of late Pleistocene ice sheet growth with realistic geography and simplified cryodynamics and geodynamics
- 1 December 1990
- journal article
- Published by Springer Nature in Climate Dynamics
- Vol. 5 (2) , 103-110
- https://doi.org/10.1007/bf00207425
Abstract
No abstract availableKeywords
This publication has 20 references indexed in Scilit:
- Growth rate of the Laurentide Ice Sheet and sea Level Lowering (with Emphasis on the 115,000 BP Sea Level Low)Published by Cambridge University Press (CUP) ,2017
- Simulations of continental ice sheet growth over the last glacial‐interglacial cycle: Experiments with a one‐level seasonal energy balance model including realistic geographyJournal of Geophysical Research: Atmospheres, 1991
- The influence of continental ice, atmospheric CO2, and land albedo on the climate of the last glacial maximumClimate Dynamics, 1987
- Global Ice-Sheet System Interlocked by Sea LevelQuaternary Research, 1986
- A Comparison of Climate Model Sensitivity with Data from the Last Glacial MaximumJournal of the Atmospheric Sciences, 1985
- CO2‐induced change in a coupled ocean‐atmosphere model and its paleoclimatic implicationsJournal of Geophysical Research: Oceans, 1985
- A coupled climate‐ice sheet model applied to the Quaternary Ice AgesJournal of Geophysical Research: Oceans, 1983
- Milankovitch Theory of Ice Ages: Hypothesis of Ice-Sheet Linkage Between Regional Insolation and Global ClimateQuaternary Research, 1983
- Simple energy balance model resolving the seasons and the continents: Application to the astronomical theory of the ice agesJournal of Geophysical Research: Oceans, 1983
- A simple parameterization for ice sheet ablation rateTellus A: Dynamic Meteorology and Oceanography, 1980