Antarctic link to deep flow speed variation during Marine Isotope Stage 3 in the western North Atlantic
The Western Boundary Undercurrent (WBUC), off eastern America, is an important component of the Atlantic Meridional Overturning circulation and is the principal route for southward transport of North Atlantic waters and southward return of Southern Source Water (SSW). Here a direct flow speed proxy...
| Main Authors: | , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
2007
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