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Abrupt climate fluctuations in the tropics: the influence of Atlantic Ocean circulation F. Alayne Street-Perrott & R. Alan Perrott
Alayne Street-Perron and Alan Perrott
are at the School of Geography, Oxford University, Mansfield Road, Oxford 0X1
3TB, UK.
Several prolonged droughts in the Sahel and tropical Mexico during the past
14,000 years were coincident with large injections of fresh water into the
northern North Atlantic Ocean. The link between these phenomena lies in the
thermohaline circulation of the oceans: input of fresh water decreases salinity
leading to reduced North Atlantic Deep Water formation and anomalies of sea
surface temperature of the kind associated with decreased rainfall in the
northern tropics. Ice-sheet disintegration, the most important source of
fresh-water input to the oceans, should therefore be considered explicitly in
models of past and future climate.
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