Advances in Differential Equations

On strong solutions of a planetary geostrophic model of the ocean

T. Tachim Medjo

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Abstract

We study, in this article, the well-posedness of a planetary geostrophic (PG) model of the ocean. This model is derived from the PG studied in [17] by adding a (non-linear) advection term in the horizontal momentum equation. We address in particular the question of existence and uniqueness of global (in time) weak solution to the model. We also discuss the asymptotic behavior of the weak solutions and the stability of the stationary solutions. We prove that any weak solution to the model converges exponentially with time to a weak solution to the primitive equations of the ocean provided that the data are small.

Article information

Source
Adv. Differential Equations Volume 13, Number 9-10 (2008), 801-828.

Dates
First available in Project Euclid: 18 December 2012

Permanent link to this document
https://projecteuclid.org/euclid.ade/1355867320

Mathematical Reviews number (MathSciNet)
MR2482578

Zentralblatt MATH identifier
1178.35295

Subjects
Primary: 86A05: Hydrology, hydrography, oceanography [See also 76Bxx, 76E20, 76Q05, 76Rxx, 76U05]
Secondary: 35A05 76D03: Existence, uniqueness, and regularity theory [See also 35Q30] 76U05: Rotating fluids

Citation

Tachim Medjo, T. On strong solutions of a planetary geostrophic model of the ocean. Adv. Differential Equations 13 (2008), no. 9-10, 801--828. https://projecteuclid.org/euclid.ade/1355867320.


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