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• W2051233573 abstract "A deep ice core extracted at Vostok station, Antarctica, provides a record of atmospheric climate and CO 2 that is representative of global changes over the last glacial‐interglacial cycle (160,000 years). Spectral analysis of the isotope temperature profile confirms the role of astronomical forcing in Quaternary climate changes. There is a remarkably close association between the climatic and CO 2 records. This association indicates a fundamental link between the climate system and the carbon cycle, although the processes involved are not clearly understood. A simple statistical comparison of the Vostok temperature record with various potential forcing factors suggests that CO 2 concentrations may have played a major role in the observed climatic record, in addition to insolation inputs exerted locally and at northern hemisphere latitudes (where continental ice sheets are growing and decaying at the glacial‐interglacial time scale). We propose that CO 2 and other atmospheric chemical changes may have had an important effect on Quaternary climate by providing, for the large 100‐kyr oscillation, the necessary amplification of the orbital forcing at that frequency." @default.
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• W2051233573 date "1988-06-28" @default.
• W2051233573 modified "2023-10-18" @default.
• W2051233573 title "Antarctic ice core: CO2 and climatic change over the last climatic cycle" @default.
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• W2051233573 doi "https://doi.org/10.1029/88eo00230" @default.
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