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Formación de aguas profundas en el Pacífico Norte durante la última terminación glacial

Y Okazaki1, A Timmermann, L Menviel

  • 1Japan Agency for Marine-Earth Science and Technology, 2-15 Natsushima-cho, Yokosuka 237-0061, Japan.

Science (New York, N.Y.)
|July 10, 2010
PubMed
Resumen

Durante la última terminación glacial, la circulación del Atlántico Norte se debilitó, causando que la formación de aguas profundas se desplazara hacia el Pacífico Norte. Este cambio en la circulación oceánica regula el transporte global de calor.

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