THE GULF STREAM AS AN INERTIAL BOUNDARY LAYER
- 15 October 1955
- journal article
- Published by Proceedings of the National Academy of Sciences in Proceedings of the National Academy of Sciences
- Vol. 41 (10) , 731-740
- https://doi.org/10.1073/pnas.41.10.731
Abstract
No abstract availableThis publication has 1 reference indexed in Scilit:
- Wind-Driven Currents in a Baroclinic Ocean; with Application to the Equatorial Currents of the Eastern PacificProceedings of the National Academy of Sciences, 1947