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 |