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Sudden changes in North Atlantic circulation during the last deglaciation

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Abstract

Sudden changes in the flow of warm Atlantic surface waters into the Norwegian Sea occurred frequently during the last deglaciation, typically involving shifts in sea surface temperature of ⩾5 °C in fewer than 40 years. These led to equally large and rapid changes in atmospheric temperatures, and to shifts in Atlantic deep thermo-haline circulation and ice-sheet melting rates.

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Authors and Affiliations

  1. Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, 02543, USA

    Scott J. Lehman & Lloyd D. Keigwin

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  1. Scott J. Lehman
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  2. Lloyd D. Keigwin
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Lehman, S., Keigwin, L. Sudden changes in North Atlantic circulation during the last deglaciation. Nature 356, 757–762 (1992). https://doi.org/10.1038/356757a0

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