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- W1997606274 abstract "By reinterpreting the “sea-ice extent” discussed in a recently proposed model of auto-oscillatory climatic change (Saltzman et al., 1981) to represent high-inertia grounded and shelf sea ice forms, instead of thinner marine ice forms, it is possible for the model to yield a much longer period of auto-oscillation, perhaps as much as 100 000 years (the dominant period of ice volume variations revealed by deep-sea ocean cores). The physical basis of the model can, in principle, be tested by future evidence regarding the long-term variations of bulk ocean temperature and atmospheric CO2 concentration." @default.
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- W1997606274 date "1982-11-01" @default.
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- W1997606274 title "A Possible Marine Mechanism for Internally Generated Long-Period Climate Cycles" @default.
- W1997606274 doi "https://doi.org/10.1175/1520-0469(1982)039<2634:apmmfi>2.0.co;2" @default.
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