On two-dimensional large-scale primitive equations in oceanic dynamics. I
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Publication:940283
DOI10.1007/s10483-007-0503-xzbMath1231.35264OpenAlexW3016894043MaRDI QIDQ940283
Publication date: 1 September 2008
Published in: Applied Mathematics and Mechanics. (English Edition) (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1007/s10483-007-0503-x
PDEs in connection with fluid mechanics (35Q35) Hydrology, hydrography, oceanography (86A05) Weak solutions to PDEs (35D30) PDEs in connection with geophysics (35Q86)
Related Items (5)
Ergodicity of two-dimensional primitive equations of large scale ocean in geophysics driven by degenerate noise ⋮ Convergence results on the boundary conditions for 2D large-scale primitive equations in oceanic dynamics ⋮ On two-dimensional large-scale primitive equations in oceanic dynamics. II ⋮ Continuous dependence of 2D large scale primitive equations on the boundary conditions in oceanic dynamics. ⋮ Time-reversal algorithms in viscoelastic media
Cites Work
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- On two-dimensional large-scale primitive equations in oceanic dynamics. II
- On the uniqueness of weak solutions of the two-dimensional primitive equations.
- Existence and regularity results for the primitive equations in two space dimensions
- Anisotropic estimates and strong solutions of the primitive equations.
- Mathematical theory for the coupled atmosphere-ocean models (CAO III)
- New formulations of the primitive equations of atmosphere and applications
- On the 2D model of large-scale atmospheric motion: well-posedness and attractors
- On the equations of the large-scale ocean
- On the Two-Dimensional Hydrostatic Navier--Stokes Equations
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