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...
Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
2001.
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Subjects: | |
Online Access: | Get fulltext |