Transport and Bottom Boundary Layer Observations of the North Atlantic Deep Western Boundary Current at the Blake Outer Ridge.

The North Atlantic Deep Western Boundary Current (DWBC) couples the global atmospheric climate to the ocean interior, making it an important component of the global climate system. Formed primarily by high-latitude deep convection, this density-driven current flows south from the Irminger Basin near...

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Bibliographic Details
Main Author: Stahr, Frederick R.
Other Authors: WASHINGTON UNIV SEATTLE APPLIED PHYSICS LAB
Format: Text
Language:English
Published: 1998
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA358708
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA358708