Name
Abstract | ||
|---|---|---|
In this paper, we derive rigorously a classical simplified model of ocean circulation,namely the so called homogeneous model of wind driven oceancirculation (see the monograph of J. Pedlosky [19]) and two of its possibleboundary layer behavior, namely Munk layers and Stommel layers.IntroductionThis paper is the fourth of a series dedicated to the derivation of some basicand classical equations of Meteorology, following the classical Physics sourcebook of J. Pedlosky [19]. It began by... |
Year | DOI | Venue |
|---|---|---|
1999 | 10.1137/S0036139997324261 | SIAM Journal on Applied Mathematics |
Keywords | Field | DocType |
wind-driven ocean circulation,homogeneous model,ocean circulation,oceanography | Meteorology,Homogeneous,Mathematical analysis,Ocean current,Geophysical fluid dynamics,Mathematics,Geophysics | Journal |
Volume | Issue | ISSN |
60 | 1 | 0036-1399 |
Citations | PageRank | References |
2 | 0.91 | 0 |
Authors | ||
2 | ||
Name | Order | Citations | PageRank |
|---|---|---|---|
| Benoît Desjardins | 1 | 2 | 0.91 |
| E. Grenier | 2 | 4 | 2.69 |