On the wind-driven circulation in an ocean with bottom topography
Open Access
- 1 January 1967
- journal article
- Published by Stockholm University Press in Tellus A: Dynamic Meteorology and Oceanography
- Vol. 19 (4), 582
- https://doi.org/10.3402/tellusa.v19i4.9825
Abstract
On the wind-driven circulation in an ocean with bottom topographyKeywords
This publication has 8 references indexed in Scilit:
- A Numerical Investigation of a Nonlinear Model of a Wind-Driven OceanJournal of the Atmospheric Sciences, 1963
- Topographic Influences on the Path of the Gulf StreamTellus A: Dynamic Meteorology and Oceanography, 1963
- A CRITERION FOR THE EXISTENCE OF INERTIAL BOUNDARY LAYERS IN OCEANIC CIRCULATIONProceedings of the National Academy of Sciences, 1962
- On the theory of the wind-driven ocean circulationJournal of Fluid Mechanics, 1962
- On the Wind-Driven Ocean CirculationTellus A: Dynamic Meteorology and Oceanography, 1956
- THE GULF STREAM AS AN INERTIAL BOUNDARY LAYERProceedings of the National Academy of Sciences, 1955
- The westward intensification of wind‐driven ocean currentsEOS, Transactions American Geophysical Union, 1948
- Wind-Driven Currents in a Baroclinic Ocean; with Application to the Equatorial Currents of the Eastern PacificProceedings of the National Academy of Sciences, 1947