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Ice ages and the thermal equilibrium of the earth

August 1, 1973

A model for climatic change, and particularly for the changes of the late Cenozoic, involves as its primary variables the albedo of the earth and the heat storage characteristics of the oceans. Geography exerts a strong influence. The model proposed does not require metaphysical causes or astronomical events other than known variations in the earth's orbit.

Publication Year 1973
Title Ice ages and the thermal equilibrium of the earth
Authors David P. Adam
Publication Type Article
Publication Subtype Journal Article
Series Title Journal of Research of the U.S. Geological Survey
Index ID 70161900
Record Source USGS Publications Warehouse