A unified asymptotic derivation of two-layer, frontal geostrophic models including planetary sphericity and variable topography
Author:
Affiliation:
1. Applied Mathematics Institute, Department of Mathematical Sciences, University of Alberta, Edmonton, Alberta T6G 2G1, Canada
Publisher
AIP Publishing
Subject
Condensed Matter Physics,Fluid Flow and Transfer Processes,Mechanics of Materials,Computational Mechanics,Mechanical Engineering
Reference28 articles.
1. B. Cushman-Roisin, “Frontal geostrophic dynamics,” J. Phys. Oceanogr. JPYOBT16, 132 (1986).
2. B. Cushman-Roisin, G. G. Sutyrin, and B. Tang, “Two-layer geostrophic dynamics. I. Governing equations,” J. Phys. Oceanogr. JPYOBT22, 117 (1992).
3. E. S. Benilov, “Large-amplitude geostrophic dynamics: The two layer model,” Geophys. Astrophys. Fluid Dyn. GAFDD366, 67 (1992).
4. G. E. Swaters, “On the baroclinic dynamics, Hamiltonian formulation and general stability characteristics of density-driven surface currents and fronts over a sloping continental shelf,” Philos. Trans. R. Soc. London, Ser. A PTRMAD345, 295 (1993).
5. Eddies in Marine Science, edited by A. R. Robinson (Springer, New York, 1983).
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