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La circulación del océano Atlántico Norte y el cambio climático abrupto durante la última glaciación

L G Henry1, J F McManus2, W B Curry3

  • 1Lamont-Doherty Earth Observatory (LDEO), Columbia University, Palisades, NY 10964, USA. lhenry@ldeo.columbia.edu.

Science (New York, N.Y.)
|July 2, 2016
PubMed
Resumen

Los cambios en la circulación oceánica impulsaron rápidos cambios climáticos durante la última edad de hielo. La reducción de la circulación de volteo del Atlántico coincidió con los períodos fríos, mientras que una circulación más fuerte trajo el calentamiento, destacando el papel clave del océano en el abrupto cambio climático glacial.

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