The cause of the ice ages

Computer Science

Scientific paper

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Scientific paper

A composite deep-sea core, normalized on the basis of sedimentary averages from seven cores from the Caribbean and one from the Pacific, reveals the occurrence of ten major glaciations during the past 730,000 years and affords a close estimate of their ages. Spacing of glaciation through time ranges from 50,000 to > 100,000 years. Obliquity minima caused significant lowering of global temperature and were important in driving the earth's climate toward a glacial mode; and obliquity maxima, especially if occurring when eccentricity was high and the earth was at perihelion during the northern summer, contributed in producing warm interglacials. Full glaciation and full deglaciation, however, appear to be primarily related to heat exchange processes between ice and ocean.

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