A two-layer frictional model of wind-driven motion in a rectangular oceanic basin
By: Pierre Welander
References
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ERMAN
, W. V., 1905, On the influence of earth's rotation on ocean currents. Arkiv f. Mafem. Astr. o. Fysik, 2, p. 11. -
MUNK
, W. H., 1950, On the wind-driven ocean cir-culation. J. Meteor., 7, pp. 75– 93. -
STOMMEL
, H., 1948, The westward intensification of wind-driven ocean currents. Trans. Amer. Geo-phys. Union, 29, pp. 202– 206. -
STOMMEL
, H., 1958, The Gulf Stream. Univ. Calif. Press and Cambr. Univ. Press. -
SVERDRUP
, H. U., 1947, Wind-driven currents in a baroclinic ocean; with application to the equa-torial currents of the eastern Pacific. Proc. Nat. Acad. Sci. Wash., 33, pp. 318– 326.
DOI: https://doi.org/10.3402/tellusa.v18i1.9183 | Journal eISSN: 3035-9554
Language: English
Page range: 54 - 62
Submitted on: Jun 28, 1965
Published on: Jan 1, 1966
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1966 Pierre Welander, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.