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- W2010076610 abstract "A probabilistic analysis of climate variation during the period AD 1050–1800 refines available estimates of the influence of temperature change on the concentration of carbon dioxide in the atmosphere. Climate warming tends to cause a net release of CO2, which in turn causes an amplification of warming. Estimates of the magnitude of this effect vary widely, leading to a wide range in global warming projections. Recent work suggested that the magnitude of this positive feedback might be about 40 parts per million by volume of CO2 per °C of warming. David Frank and colleagues use three Antarctic ice cores and a suite of climate reconstructions to show that the feedback is likely to be much smaller, with a median of only about 8 p.p.m.v. CO2 per °C." @default.
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- W2010076610 date "2010-01-27" @default.
- W2010076610 modified "2023-10-12" @default.
- W2010076610 title "Degrees of climate feedback" @default.
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- W2010076610 doi "https://doi.org/10.1038/463438a" @default.
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