## Abstract It is generally believed that the increasing CO~2~ content of the atmosphere will lead to a substantial climatic warming in the polar regions. In this study the effect of consequent changes in the ice accumulation rate over the Antarctic Ice Sheet is investigated by means of a numerical
A model study of the role of variable ice albedo in the climate response of the earth to orbital variations
β Scribed by G.E. Birchfield; Johannes Weertman
- Publisher
- Elsevier Science
- Year
- 1982
- Tongue
- English
- Weight
- 762 KB
- Volume
- 50
- Category
- Article
- ISSN
- 0019-1035
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