Transports of water masses through the Faroese Channels determined by an inverse method
- 30 April 1988
- journal article
- Published by Elsevier in Deep Sea Research Part A. Oceanographic Research Papers
- Vol. 35 (4) , 595-617
- https://doi.org/10.1016/0198-0149(88)90133-1
Abstract
No abstract availableThis publication has 8 references indexed in Scilit:
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- ReplyJournal of Physical Oceanography, 1986
- Comments on “Can a Tracer Field Be Inverted for Velocity?”Journal of Physical Oceanography, 1986
- Can a Tracer Field Be Inverted for Velocity?Journal of Physical Oceanography, 1985
- Circulation and Heat Flux in the Bermuda TriangleJournal of Physical Oceanography, 1983
- Variational inverse method for study of oceanic circulationDeep Sea Research Part A. Oceanographic Research Papers, 1981
- Circulation and water masses in the Faroese Channels during overflow '73Ocean Dynamics, 1981
- The North Atlantic general circulation west of 50°W determined by inverse methodsReviews of Geophysics, 1978