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Published on: September 5, 2018
Flujo inverso de las aguas profundas del Atlántico durante el último máximo glacial
César Negre1, Rainer Zahn, Alexander L Thomas
1Institut de Ciència i Tecnologia Ambientals (ICTA), Universitat Autònoma de Barcelona, 08193 Bellaterra, Spain. cesar@negre.us
Nature
|November 5, 2010
Resumen
La circulación de volcado meridional del Atlántico (MOC) puede haberse invertido durante el Último Máximo Glacial, con aguas profundas que fluyen hacia el norte desde el Océano Antártico, a diferencia del patrón actual.
Área de la Ciencia:
- La paleoceanografía es la paleoceanografía.
- Ciencias del clima Ciencias del clima Ciencias del clima Ciencias del clima
- Oceanografía La oceanografía es la oceanografía.
Sus antecedentes:
- La circulación de volteo meridional del Atlántico (MOC) es crucial para el clima global, redistribuyendo el calor y ventilando las profundidades del océano.
- Se debate el comportamiento del MOC pasado, especialmente durante el Último Máximo Glacial, con pruebas contradictorias de proxies.
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