A coupled climate- ice sheet model applied to the Quaternary ice ages.

Research output: Contribution to journalArticle

61 Scopus citations

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 languageEnglish (US)
Pages (from-to)7705-7718
Number of pages14
JournalJournal of Geophysical Research
Volume88
Issue numberC12
DOIs
StatePublished - Jan 1 1983

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Forestry
  • Oceanography
  • Aquatic Science
  • Ecology
  • Water Science and Technology
  • Soil Science
  • Geochemistry and Petrology
  • Earth-Surface Processes
  • Atmospheric Science
  • Space and Planetary Science
  • Earth and Planetary Sciences (miscellaneous)
  • Palaeontology

Fingerprint Dive into the research topics of 'A coupled climate- ice sheet model applied to the Quaternary ice ages.'. Together they form a unique fingerprint.

  • Cite this