Numerical evidence against reversed thermohaline circulation in the warm Paleocene/Eocene ocean

The question of whether deep water formation might have occurred in subtropical latitudes in the early Cenozoic is examined through use of a global ocean model forced by mixed boundary conditions. Zonal mean surface temperatures and wind stresses are derived from an atmospheric general circulation m...

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Bibliographic Details
Main Authors: Bice, Karen L. (Author), Marotzke, Jochem (Author)
Format: Article
Published: 2001.
Online Access:Get fulltext

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