Coupled wind-forced controls of the Bering–Chukchi shelf circulation and the Bering Strait throughflow: Ekman transport, continental shelf waves, and variations of the Pacific–Arctic sea surface height gradient

Author:

Danielson Seth L.,Weingartner Thomas J.,Hedstrom Katherine S.,Aagaard Knut,Woodgate Rebecca,Curchitser Enrique,Stabeno Phyllis J.

Funder

ConocoPhillips

Shell

DOI-BOEM

NSF

NPRB

Publisher

Elsevier BV

Subject

Geology,Aquatic Science

Reference111 articles.

1. The role of sea–ice and other fresh water in the Arctic Circulation;Aagaard;Journal of Geophysical Research: Oceans,1989

2. On the halocline of the Arctic Ocean;Aagaard;Deep Sea Research Part A,1981

3. On the wind-driven variability of the flow through Bering Strait;Aagaard;Journal of Geophysical Research: Oceans,1985

4. Some controls on flow and salinity in Bering Strait;Aagaard;Geophysical Research Letters,2006

5. Continental Shelf waves and alongshore variations in bottom topography and coastline;Allen;Journal of Physical Oceanography,1976

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