Pages that link to "Item:Q329258"
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The following pages link to Global strong \(L^{p}\) well-posedness of the 3D primitive equations with heat and salinity diffusion (Q329258):
Displaying 24 items.
- Strong solutions to the 3D primitive equations with only horizontal dissipation: near \(H^{1}\) initial data (Q524257) (← links)
- Local and global well-posedness of strong solutions to the 3D primitive equations with vertical Eddy diffusivity (Q742791) (← links)
- Global wellposedness of the primitive equations with nonlinear equation of state in critical spaces (Q831431) (← links)
- Global well-posedness for the primitive equations with less regular initial data (Q1000291) (← links)
- The primitive equations as the small aspect ratio limit of the Navier-Stokes equations: rigorous justification of the hydrostatic approximation (Q1732991) (← links)
- Global well-posedness of the ocean primitive equations with nonlinear thermodynamics (Q2050576) (← links)
- The primitive equations in the scaling-invariant space \(L^{\infty}(L^1)\) (Q2064546) (← links)
- Continuous dependence of 2D large scale primitive equations on the boundary conditions in oceanic dynamics. (Q2076582) (← links)
- Global well-posedness of the 3D primitive equations with horizontal viscosity and vertical diffusivity (Q2127400) (← links)
- The hydrostatic Stokes semigroup and well-posedness of the primitive equations on spaces of bounded functions (Q2182584) (← links)
- Convergence results on the boundary conditions for 2D large-scale primitive equations in oceanic dynamics (Q2195494) (← links)
- Global well-posedness for the 3D primitive equations in anisotropic framework (Q2287328) (← links)
- Global strong well-posedness of the three dimensional primitive equations in \({L^p}\)-spaces (Q2630263) (← links)
- The primitive equations approximation of the anisotropic horizontally viscous \(3D\) Navier-Stokes equations (Q2664928) (← links)
- Rigorous derivation of the full primitive equations by the scaled Boussinesq equations with rotation (Q2699577) (← links)
- Analysis of Viscous Fluid Flows: An Approach by Evolution Equations (Q3296719) (← links)
- Global well-posedness of <i>z</i>-weak solutions to the primitive equations without vertical diffusivity (Q5056855) (← links)
- Rigorous justification of the hydrostatic approximation for the primitive equations by scaled Navier–Stokes equations* (Q5136535) (← links)
- Bounded 𝐻^{∞}-calculus for the hydrostatic Stokes operator on 𝐿^{𝑝}-spaces and applications (Q5274744) (← links)
- Data assimilation to the primitive equations with \(L^p\)-\(L^q\)-based maximal regularity approach (Q6144337) (← links)
- On the rigorous mathematical derivation for the viscous primitive equations with density stratification (Q6159422) (← links)
- The primitive equations with stochastic wind driven boundary conditions (Q6202714) (← links)
- Global wellposedness of the primitive equations with nonlinear equation of state in critical spaces (Q6614860) (← links)
- The hydrostatic approximation of the Boussinesq equations with rotation in a thin domain (Q6650549) (← links)