INFLUENCE OF THE CLIMAP ICE SHEET ON THE CLIMATE OF A GENERAL CIRCULATION MODEL; IMPLICATIOtilS FOR THE MILANKOVITCH THEORY
While the spectral analys:is of data from deep sea cores supports the suggestion that the temporal variation of the earth's orbital parameters is responsib,le for triggering the growth and decay of continental ice duri.ng the Quaternary (1)
Main Authors: | , |
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Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.143.4441 http://www.gfdl.noaa.gov/reference/bibliography/1984/ajb8401.pdf |
Summary: | While the spectral analys:is of data from deep sea cores supports the suggestion that the temporal variation of the earth's orbital parameters is responsib,le for triggering the growth and decay of continental ice duri.ng the Quaternary (1) |
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