Pages that link to "Item:Q4303874"
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The following pages link to Numerical analysis of the coupled atmosphere-ocean models (CAO II) (Q4303874):
Displaying 50 items.
- Global strong \(L^{p}\) well-posedness of the 3D primitive equations with heat and salinity diffusion (Q329258) (← 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)
- Analysis, modelling, optimization, and numerical techniques. ICAMI, San Andres Island, Colombia, November 2013 (Q476922) (← 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)
- 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)
- 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)
- Interface flux recovery coupling method for the ocean-atmosphere system (Q780030) (← links)
- The primitive equations of the ocean with delays (Q837668) (← links)
- A two-grid finite difference method for the primitive equations of the ocean (Q943730) (← 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)
- 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)
- Primitive equations with half horizontal viscosity (Q2025725) (← links)
- The primitive equations in the scaling-invariant space \(L^{\infty}(L^1)\) (Q2064546) (← links)
- A linear, stabilized, non-spatial iterative, partitioned time stepping method for the nonlinear Navier-Stokes/Navier-Stokes interaction model (Q2108335) (← links)
- An unconditionally stable, high-order and flux-conservative fluid-fluid coupling method (Q2122035) (← links)
- Existence of a strong solution to moist atmospheric equations with the effects of topography (Q2126627) (← 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)
- The hydrostatic Stokes semigroup and well-posedness of the primitive equations on spaces of bounded functions (Q2182584) (← links)
- A projection based variational multiscale method for a fluid-fluid interaction problem (Q2184280) (← 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)
- Phase transition models in atmospheric dynamics (Q2254956) (← links)
- New approach to prove the stability of a decoupled algorithm for a fluid-fluid interaction problem (Q2297138) (← links)
- A regularity-aware algorithm for variational data assimilation of an idealized coupled atmosphere-ocean model (Q2311985) (← links)
- Stability of weak solutions for the large-scale atmospheric equations (Q2405738) (← links)
- Numerical approximation of atmospheric-ocean models with subdivision algorithm (Q2455012) (← links)
- On the order of magnitude of the baroclinic flow in the primitive equations of the ocean (Q2504900) (← links)
- A stabilized finite element method for the Stokes-Stokes coupling interface problem (Q2670710) (← links)
- Stability analysis of coupled advection-diffusion models with bulk interface condition (Q2676799) (← links)
- Small-time solvability of the primitive equations for the coupled atmosphere and ocean model (Q2693078) (← links)
- A spectral coupled ocean-atmosphere model (Q2730439) (← links)
- Numerical estimates of mechanical energy transfer from the atmosphere to the Indian ocean (Q2838927) (← links)
- A fluid-fluid interaction method using decoupled subproblems and differing time steps (Q2910811) (← links)
- (Q3149653) (← links)
- Models of the coupled atmosphere and ocean (CAO I) (Q4303875) (← links)