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On the use of a two-layer fluid stratification model in studies of topographically-generated baroclinic tides

✍ Scribed by Vlasenko, V. I. ;Stashchuk, N. M.

Book ID
112736283
Publisher
Springer-Verlag
Year
1991
Weight
309 KB
Volume
2
Category
Article
ISSN
0920-5047

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## Abstract Numerical experiments with a two‐level, quasi‐geostrophic model, described by Davies and Davies (1969), have been extended in several ways; the grid spacing of the previous model has been halved, greatly reducing numerical errors, and the lateral East‐West span of the flow domain is muc