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- W2069012742 abstract "A box model of the atmosphere and ocean mixed-layer, overlying an advective-diffusive deep ocean, is used to investigate the coupled effect of a changing rate of ocean water overturning on atmospheric temperature and carbon concentration. Under the assumption that overturning slows down with increasing temperatures, a long-term detrimental feedback is possible via enhanced greenhouse forcing, whereas the beneficial feedback (cooling trend) previously discussed by other authors seems to prevail in the short term (e.g., one to three centuries)." @default.
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- W2069012742 date "1996-06-01" @default.
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- W2069012742 title "Preliminary assessment of the potential coupling between atmospheric temperature and CO2 concentration via ocean water overturning" @default.
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- W2069012742 doi "https://doi.org/10.1016/0196-8904(95)00295-2" @default.
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