Wind-driven circulation in one- and two-layer oceans of variable depth
Open Access
- 1 February 1968
- journal article
- Published by Stockholm University Press in Tellus
- Vol. 20 (1), 1-16
- https://doi.org/10.1111/j.2153-3490.1968.tb00347.x
Abstract
Wind-driven circulation in one- and two-layer oceans of variable depthKeywords
This publication has 9 references indexed in Scilit:
- On the wind-driven circulation in an ocean with bottom topographyTellus A: Dynamic Meteorology and Oceanography, 1967
- The theory of free inertial currents: I. Path and structureTellus A: Dynamic Meteorology and Oceanography, 1967
- A two-layer frictional model of wind-driven motion in a rectangular oceanic basinTellus A: Dynamic Meteorology and Oceanography, 1966
- The Gulf StreamPublished by University of California Press ,1965
- Some effects of stratification and geometry in rotating fluidsJournal of Fluid Mechanics, 1965
- On the general theory of contained rotating fluid motionsJournal of Fluid Mechanics, 1965
- A CRITERION FOR THE EXISTENCE OF INERTIAL BOUNDARY LAYERS IN OCEANIC CIRCULATIONProceedings of the National Academy of Sciences, 1962
- ON THE WIND-DRIVEN OCEAN CIRCULATIONJournal of Meteorology, 1950
- The westward intensification of wind‐driven ocean currentsEOS, Transactions American Geophysical Union, 1948