Pages that link to "Item:Q4303875"

The following pages link to Models of the coupled atmosphere and ocean (CAO I) (Q4303875):

Displaying 50 items.

• Existence and regularity results for the inviscid primitive equations with lateral periodicity (Q301540) (← 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)
• Global attractor of atmospheric circulation equations with humidity effect (Q448598) (← links)
• On unique ergodicity in nonlinear stochastic partial differential equations (Q526583) (← links)
• Non-autonomous planetary 3D geostrophic equations with oscillating external force and its global attractor (Q533029) (← links)
• Pathwise solutions of the 2-D stochastic primitive equations (Q538477) (← 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)
• Local existence and uniqueness for the hydrostatic Euler equations on a bounded domain (Q618288) (← 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)
• 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)
• Numerical solutions of a robust control problem associated with the quasi-geostrophic equation of the ocean (Q697024) (← links)
• Maximum principle of optimal control of the primitive equations of the ocean with two point boundary state constraint (Q708863) (← links)
• Validating and assessing the sensitivity of the climate model with an ocean general circulation model developed at the Institute of Atmospheric Physics, Russian Academy of Sciences (Q731778) (← 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 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)
• Regularity results for Stokes type systems related to climatology (Q1346857) (← links)
• On mathematical problems for the primitive equations of the ocean: The mesoscale midlatitude case (Q1570944) (← links)
• Existence of a strong solution and trajectory attractor for a climate dynamics model with topography effects (Q1674416) (← links)
• Random attractor for the 3D viscous primitive equations driven by fractional noises (Q1732149) (← links)
• Finite dimensionality of global attractor for the solutions to 3D viscous primitive equations of large-scale moist atmosphere (Q1756883) (← links)
• Asymptotic analysis of the primitive equations under the small depth assumption (Q1776946) (← links)
• A basic reference state suitable for anomaly-coupled ocean-atmosphere climate models (Q1809009) (← links)
• Stratified models in geophysical fluid mechanics (Q1826252) (← links)
• Mathematical theory for the coupled atmosphere-ocean models (CAO III) (Q1914528) (← links)
• Finite volume multilevel approximation of the shallow water equations (Q1943072) (← links)
• Steady state solution to atmospheric circulation equations with humidity effect (Q1952968) (← links)
• Primitive equations with horizontal viscosity: the initial value and the time-periodic problem for physical boundary conditions (Q2030810) (← links)
• Local existence and uniqueness of strong solutions to the two dimensional compressible primitive equations with density-dependent viscosity (Q2050585) (← links)
• Continuous dependence of 2D large scale primitive equations on the boundary conditions in oceanic dynamics. (Q2076582) (← links)
• Global well-posedness of stochastic 2D primitive equations with random initial conditions (Q2116284) (← links)
• An unconditionally stable, high-order and flux-conservative fluid-fluid coupling method (Q2122035) (← links)
• NS-\(\omega\) model for fluid-fluid interaction problems at high Reynolds numbers (Q2142215) (← links)
• Approximate deconvolution models for a fluid-fluid interaction problem with high Reynolds numbers (Q2147302) (← links)
• A projection based variational multiscale method for a fluid-fluid interaction problem (Q2184280) (← links)
• Stochastic 2D primitive equations: central limit theorem and moderate deviation principle (Q2203788) (← links)
• Defect-deferred correction method based on a subgrid artificial viscosity model for fluid-fluid interaction (Q2227684) (← links)
• Organization of numerical experiments with an atmospheric general circulation model and an ocean global model (Q2245898) (← links)
• A grad-div stabilized penalty projection algorithm for fluid-fluid interaction (Q2247116) (← links)
• New approach to prove the stability of a decoupled algorithm for a fluid-fluid interaction problem (Q2297138) (← links)
• Regularity of global attractor for atmospheric circulation equations with humidity effect (Q2300525) (← links)