Desjardins, B.; Grenier, E. On the homogeneous model of wind-driven ocean circulation. (English) Zbl 0958.76092 SIAM J. Appl. Math. 60, No. 1, 43-60 (1999). The paper contains a formal derivation of the quasigeostrophic equations on \(\beta\)-plane, and the derivation of the corresponding boundary layers, as is well known since J. Pedlosky [Geophysical fluid dynamics. 2nd ed. (Study ed.). New York etc.: Springer-Verlag. XIV (1987; Zbl 0713.76005)]. Reviewer: G.Zimmermann (Mainz) Cited in 3 ReviewsCited in 24 Documents MSC: 76U05 General theory of rotating fluids 86A05 Hydrology, hydrography, oceanography 86A10 Meteorology and atmospheric physics Keywords:wind-driven ocean circulation; beta-plane; quasigeostrophic equations; boundary layers Citations:Zbl 0713.76005 PDFBibTeX XMLCite \textit{B. Desjardins} and \textit{E. Grenier}, SIAM J. Appl. Math. 60, No. 1, 43--60 (1999; Zbl 0958.76092) Full Text: DOI