2009
DOI: 10.1093/imrn/rnp004
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Rotating Fluids with Small Viscosity

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Cited by 14 publications
(29 citation statements)
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“…We remark that, if ν ∼ ν ∼ ε α , then unlike the case of rotating fluids ( [35]) where the limit system is zero, the limit system of the primitive equations, when ε goes to zero, is the inviscid quasi-geostrophic system, which has no regularizing effect. So we have to estimate the H σ -norm, with σ > 5 2 , of the solution of the quasi-geostrophic system.…”
Section: Theorem 12 (Local Existencementioning
confidence: 88%
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“…We remark that, if ν ∼ ν ∼ ε α , then unlike the case of rotating fluids ( [35]) where the limit system is zero, the limit system of the primitive equations, when ε goes to zero, is the inviscid quasi-geostrophic system, which has no regularizing effect. So we have to estimate the H σ -norm, with σ > 5 2 , of the solution of the quasi-geostrophic system.…”
Section: Theorem 12 (Local Existencementioning
confidence: 88%
“…The idea is to carefully study the dependence with respect to the cut-off radii r and R of the constant C r,R arising in the Strichartz estimates in order to get an estimate which is able to absorb the blowing-up term 1 ε α . The goal of this paper is to extend the result obtained in [35] to the primitive equations (AP E ε ) and to show global existence of strong solutions of (AP E ε ) for large data when ε is small enough, in the case where ν = ε α , ν = ρε α for α ≤ α 0 and without any particular assumption on ρ. We will adapt the computations of eigenvalues and eigenvectors of the linearized primitive equations developed by F.Charve in [8], [7], [9], and [10] in the isotropic case to the anisotropic case.…”
Section: Theorem 12 (Local Existencementioning
confidence: 88%
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