Fluctuating winds and the ocean circulation
Open Access
- 1 May 1967
- journal article
- Published by Stockholm University Press in Tellus
- Vol. 19 (2) , 250-257
- https://doi.org/10.1111/j.2153-3490.1967.tb01480.x
Abstract
The fluctuating and steady response of a simple bounded ocean model to a surface wind stress which oscillates at or near one of the Rossby wave resonance frequencies of the basin is computed under the assumption that the response is limited by finite amplitude effects. It is shown that oscillations of the normal modes can never rectify in a way to produce intense boundary currents, but that motions driven not at a resonance frequency are able to produce such steady boundary layers. DOI: 10.1111/j.2153-3490.1967.tb01480.xKeywords
This publication has 2 references indexed in Scilit:
- A Study of the Time Dependent Ocean CirculationJournal of the Atmospheric Sciences, 1965
- CIX. A Technique for rendering approximate solutions to physical problems uniformly validJournal of Computers in Education, 1949