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: https://doi.org/10.3402/tellusa.v19i2.9784 | Journal eISSN: 3035-9554
Language: English
Page range: 250 - 257
Submitted on: Jan 17, 1966
Published on: Jan 1, 1967
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1967 Joseph Pedlosky, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.