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)

Bibliographic Details
Main Authors: S. Manabe, A. J. Broccoli
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Ice Sheet
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
Description
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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