Non-linear theory of a wind-driven homogeneous layer near the equator
- 31 December 1960
- journal article
- Published by Elsevier in Deep Sea Research (1953)
- Vol. 6, 303-310
- https://doi.org/10.1016/0146-6313(59)90089-9
Abstract
No abstract availableKeywords
This publication has 5 references indexed in Scilit:
- The Equatorial Undercurrent in the Light of the Vorticity EquationTellus, 1955
- On the fine-structure of the Gulf stream frontDeep Sea Research (1953), 1955
- Lateral eddy viscosity in the Gulf stream systemDeep Sea Research (1953), 1955
- Three Detailed Cross-Sections of the Gulf Stream.Tellus, 1954
- The Wind-driven Circulation in Ocean Basins of Various ShapesTellus, 1950