“Slow” physics of large continental ice sheets and underlying bedrock and its relation to the Pleistocene ice ages
Authors:
- G. Edward BirchfieldGBG. Edward Birchfield
- Robert W. GrumbineRGRobert W. Grumbine
- 1 January 1985
- journal article
- research article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 90 (B13) , 11294-11302
Abstract
No abstract availableThis publication has 24 references indexed in Scilit:
- A theoretical framework for the Pleistocene ice agesJournal of the Geological Society, 1985
- On Long-Period Internal Oscillations in a Simple Climate Model with an Ice Sheet (Abstract)Annals of Glaciology, 1984
- Focal depths of intracontinental and intraplate earthquakes and their implications for the thermal and mechanical properties of the lithosphereJournal of Geophysical Research, 1983
- Lithosphere deformation by continental ice sheetsProceedings of the Royal Society of London. A. Mathematical and Physical Sciences, 1981
- A climate model with cryodynamics and geodynamicsJournal of Geophysical Research: Oceans, 1981
- A Paleoclimate Model of Northern Hemisphere Ice SheetsQuaternary Research, 1981
- Long-Term Variations of Daily Insolation and Quaternary Climatic ChangesJournal of the Atmospheric Sciences, 1978
- A study of the stability of a model continental ice sheet subject to periodic variations in heat inputJournal of Geophysical Research, 1977
- Variations in the Earth's Orbit: Pacemaker of the Ice AgesScience, 1976
- Insolation changes, ice volumes, and the O18 record in deep‐sea coresReviews of Geophysics, 1970