Convergence results on the boundary conditions for 2D large-scale primitive equations in oceanic dynamics
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Publication:2195494
DOI10.1155/2020/6919725zbMath1459.86008OpenAlexW3043757329MaRDI QIDQ2195494
Publication date: 26 August 2020
Published in: Discrete Dynamics in Nature and Society (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1155/2020/6919725
Cites Work
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- Continuous dependence for the nonhomogeneous Brinkman-Forchheimer equations in a semi-infinite pipe
- Global strong \(L^{p}\) well-posedness of the 3D primitive equations with heat and salinity diffusion
- Convergence results for Forchheimer's equations for fluid flow in porous media
- On two-dimensional large-scale primitive equations in oceanic dynamics. I
- On two-dimensional large-scale primitive equations in oceanic dynamics. II
- On the 3D viscous primitive equations of the large-scale atmosphere
- Existence and regularity results for the primitive equations in two space dimensions
- Continuous dependence for a thermal convection model with temperature-dependent solubility
- Continuous dependence on boundary reaction terms in a porous medium of Darcy type
- Global attractor of the three-dimensional primitive equations of large-scale Ocean and atmosphere dynamics
- Continuous dependence for the Brinkman-Forchheimer fluid interfacing with a Darcy fluid in a bounded domain
- Sharp well-posedness and ill-posedness of the three-dimensional primitive equations of geophysics in Fourier-Besov spaces
- Existence and non-uniqueness of global weak solutions to inviscid primitive and Boussinesq equations
- Global well-posedness of the three-dimensional viscous primitive equations of large scale ocean and atmosphere dynamics
- Global well-posedness for the viscous primitive equations of geophysics
- Continuous dependence on the reaction terms in porous convection with surface reactions
- New formulations of the primitive equations of atmosphere and applications
- On the equations of the large-scale ocean
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