Climatic warming and basal melting of large ice sheets: Possible implications for east Antarctica

Geophysical Research Letters

Volumn 14, Issue 1, 1987, Pages 33-36

  Saari, Marc R ^a   Yuen, David A ^b   Schubert, Gerald ^c  

^a ARIZONA STATE UNIVERSITY   (United States)

^b UNIVERSITY OF MINNESOTA   (United States)

^c UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0023467133     PISSN: 00948276     EISSN: 19448007     Source Type: Journal    
DOI: 10.1029/GL014i001p00033     Document Type: Article

References (23)

1. The relation of deep sea sedimentation rates to variations in climate
2. Strain heating and creep instability in glaciers and ice sheets
3. The surface of the ice‐age earth
4. The geologic record of climate change
5. Measured Antarctic ice sheet: surface configuration, ice thickness, volume and bedrock
6. The existence of multiple steady states in the flow of large ice masses
7. The uniqueness of steady state flows of glaciers and ice sheets
8. Modeling the ice‐age climate
9. Changing climate: Geothermal evidence from permafrost in the Alaskan arctic
10. Lateglacial maximum‐Holocene atmospheric and ice‐thickness changes from Antarctic ice‐core studies
11. Initiation of ice ages by creep instability and surging of the East Antarctic ice sheet
12. The oxygen isotope stratigraphic record of the Late Pleistocene
13. Trace gases and other potential perturbations to global climate
14. Reaction of the accumulation zone portions of glaciers to climatic change
15. Origin of ice ages: an ice shelf theory for Pleistocene glaciation
16. The role of shear heating in the dynamics of large ice masses