Abstract
An analytic solution for the three-dimensional structure of horizontal velocity has been computed for a parallelepipedic model ocean with certain restrictions. Observed features that repeated themselves when the model parameters were changed have been generalized, and it is hypothesized that some of the persistent features obtained from the computations exist in the real ocean.
Recommended Citation
Hassan, El Sayed M.. 1964. "The general oceanic circulation; Some computations, a working hypothesis, and proposed tests." Journal of Marine Research 22, (2). https://elischolar.library.yale.edu/journal_of_marine_research/1025
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