Pages that link to "Item:Q1914528"

The following pages link to Mathematical theory for the coupled atmosphere-ocean models (CAO III) (Q1914528):

Displaying 50 items.

• Global well-posedness of strong solutions to a tropical climate model (Q262117) (← links)
• Zero viscosity limit for analytic solutions of the primitive equations (Q303700) (← links)
• Averaging of the planetary 3D geostrophic equations with oscillating external forces (Q434604) (← links)
• Small-time existence of a strong solution of primitive equations for the ocean (Q447808) (← links)
• Local well-posedness for the tropical climate model with fractional velocity diffusion (Q510033) (← links)
• Strong solutions to the 3D primitive equations with only horizontal dissipation: near \(H^{1}\) initial data (Q524257) (← links)
• Non-autonomous planetary 3D geostrophic equations with oscillating external force and its global attractor (Q533029) (← links)
• Global strong solutions of Navier-Stokes equations with interface boundary in three-dimensional thin domains (Q544163) (← links)
• Existence of the universal attractor for the 3-D viscous primitive equations of large-scale moist atmosphere (Q549224) (← links)
• The exponential behavior of the stochastic three-dimensional primitive equations with multiplicative noise (Q619705) (← links)
• Second-order optimality conditions for optimal control of the primitive equations of the ocean with periodic inputs (Q626427) (← links)
• Partitioned time discretization for parallel solution of coupled ODE systems (Q634118) (← links)
• Error estimates of a decoupled algorithm for a fluid-fluid interaction problem (Q679593) (← links)
• Stability of algorithms for a two domain natural convection problem and observed model uncertainty (Q695709) (← links)
• Maximum principle of optimal control of the primitive equations of the ocean with two point boundary state constraint (Q708863) (← links)
• Local and global well-posedness of strong solutions to the 3D primitive equations with vertical Eddy diffusivity (Q742791) (← links)
• Global well-posedness of strong solutions to the 3D primitive equations with horizontal eddy diffusivity (Q743891) (← links)
• Interface flux recovery coupling method for the ocean-atmosphere system (Q780030) (← links)
• The primitive equations of the ocean with delays (Q837668) (← links)
• 3D stochastic primitive equations of the large-scale ocean: Global well-posedness and attractors (Q842406) (← links)
• On two-dimensional large-scale primitive equations in oceanic dynamics. I (Q940283) (← links)
• On strong solutions of the multi-layer quasi-geostrophic equations of the ocean (Q943772) (← links)
• On the uniqueness of \(z\)-weak solutions of the three-dimensional primitive equations of the ocean (Q974549) (← links)
• Optimal control of the primitive equations of the ocean with state constraints (Q984034) (← links)
• Pullback attractors for closed cocycles (Q988160) (← links)
• Pontryagin's maximum principle for optimal control of the stationary primitive equations of the ocean (Q1021744) (← links)
• On mathematical problems for the primitive equations of the ocean: The mesoscale midlatitude case (Q1570944) (← links)
• The finiteness of determining degrees of freedom for the quasi-geostrophic multi-layer ocean model (Q1587225) (← links)
• Continuous data assimilation for the 3D primitive equations of the ocean (Q1633406) (← links)
• Existence of a strong solution and trajectory attractor for a climate dynamics model with topography effects (Q1674416) (← links)
• Markov selection and \(W\)-strong Feller for 3D stochastic primitive equations (Q1703885) (← links)
• Random attractor for the 3D viscous primitive equations driven by fractional noises (Q1732149) (← links)
• The primitive equations as the small aspect ratio limit of the Navier-Stokes equations: rigorous justification of the hydrostatic approximation (Q1732991) (← links)
• On the finite element approximation for non-stationary saddle-point problems (Q1756711) (← links)
• Interface boundary value problem for the Navier-Stokes equations in thin two-layer domains (Q1763675) (← links)
• Stratified models in geophysical fluid mechanics (Q1826252) (← links)
• Robin-type boundary control problems for the nonlinear Boussinesq type equations (Q1856796) (← links)
• First order decoupled method of the primitive equations of the ocean: I: Time discretization (Q2019169) (← links)
• Finite-time blowup and ill-posedness in Sobolev spaces of the inviscid primitive equations with rotation (Q2020130) (← links)
• Global well-posedness of strong solutions to the 2D nonhomogeneous incompressible primitive equations with vacuum (Q2020132) (← links)
• Navier-Stokes equations in a curved thin domain. III: Thin-film limit (Q2025723) (← links)
• Local existence and uniqueness of strong solutions to the two dimensional compressible primitive equations with density-dependent viscosity (Q2050585) (← links)
• Hydrostatic approximation of the 2D MHD system in a thin strip with a small analytic data (Q2075193) (← links)
• Continuous dependence of 2D large scale primitive equations on the boundary conditions in oceanic dynamics. (Q2076582) (← links)
• Continuous boundary condition at the interface for two coupled fluids (Q2080850) (← links)
• Global well-posedness of stochastic 2D primitive equations with random initial conditions (Q2116284) (← links)
• Existence of a strong solution to moist atmospheric equations with the effects of topography (Q2126627) (← links)
• Global well-posedness of the 3D primitive equations with horizontal viscosity and vertical diffusivity (Q2127400) (← links)
• Uniform stability and convergence of the iterative solutions of the 3D steady viscous primitive equations of the ocean under the small depth assumption (Q2161506) (← links)
• On the hydrostatic approximation of compressible anisotropic Navier-Stokes equations-rigorous justification (Q2162744) (← links)