References
- CHARNEY, J. G., 1955: The Gulf Stream as an inertial boundary layer. Proc. N.A.S. (USA). 41, No. 10, pp. 731–740.
- MONTGOMERY, R. B., 1940: The present evidence on the importance of lateral mixing processes in the Ocean. Bull. Amer. Met. Soc. 21, p. 87.
- MONK, W. H., 1950: On the wind-driven ocean circulation. J. Met. 7, p. 79.
- MUNK, W. H., and CARRIER, G. F., 1950: The wind-driven circulation in ocean basins of various shapes. Tellus, 2, No. 3, pp. 158–167.
- STOMMEL, H., is: Discussion published as a supplement to the Journal of Marine Research, 54, No. 4. Also, “Why do our ideas about the ocean circulation have such a peculiarly dream-like quality?”, April 1954.
- SVERDRUP, A. U., 1947: Wind-driven currents in a baroclinic ocean with application to the equatorial currents of the Eastern Pacific. Proc. N.A.S. (USA) 33, P. 358.