Abstract
The simplest problem in the formation of an inertial stratified western-boundary current on a continental shelf is examined by numerical treatment of the three-dimensional conservation equations. An offshore countercurrent appears as the predominant feature of the flow.
Recommended Citation
Niiler, P. P., and S. L. Spiegel. 1968. "Formation of an inertial current on a continental shelf." Journal of Marine Research 26, (1). https://elischolar.library.yale.edu/journal_of_marine_research/1110
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