Abstract
A coupled climate-ice sheet model is used in an attempt to simulate the N hemisphere ice-sheet volume variations implied by deep-sea core records over the last several 105 years. The lack of sea-ice variations causes the biggest departures from the GCM results. The two types of models produce similar ice-age simulations over the last 700 kyr in response to the orbital perturbations. In particular, fairly realistic simulations with strong 100kyr cycles similar to those obtained by adding an ice-calving mechanism to the ice-sheet model in Pollard (1982) are again produced in the coupled model. -from Author
| Original language | English (US) |
|---|---|
| Pages (from-to) | 7705-7718 |
| Number of pages | 14 |
| Journal | Journal of Geophysical Research |
| Volume | 88 |
| Issue number | C12 |
| DOIs | |
| State | Published - 1983 |
All Science Journal Classification (ASJC) codes
- Forestry
- Aquatic Science
- Soil Science
- Water Science and Technology
- Earth-Surface Processes
- Geochemistry and Petrology
- Geophysics
- Oceanography
- Palaeontology
- Ecology
- Earth and Planetary Sciences (miscellaneous)
- Space and Planetary Science
- Atmospheric Science
