Pages that link to "Item:Q4729571"

The following pages link to Existence of Solutions to the Stommel–Charney Model of the Gulf Stream (Q4729571):

Displaying 32 items.

• Trajectory attractors for non-autonomous dissipative 2d Euler equations (Q256796) (← links)
• A two-level finite element discretization of the streamfunction formulation of the stationary quasi-geostrophic equations of the ocean (Q316202) (← links)
• Infinite energy solutions for dissipative Euler equations in \(\mathbb{R}^2\) (Q498805) (← links)
• Strong trajectory and global \(\mathbf{W^{1,p}}\)-attractors for the damped-driven Euler system in \(\mathbb R^2\) (Q520936) (← links)
• Strong trajectory attractors for dissipative Euler equations (Q640016) (← links)
• Numerical solutions of a robust control problem associated with the quasi-geostrophic equation of the ocean (Q697024) (← links)
• The steady state solutions to thermohaline circulation equations (Q727937) (← links)
• Roughness-induced effects on the quasi-geostrophic model (Q852099) (← links)
• Upper bounds for the attractor dimension of damped Navier-Stokes equations in \(\mathbb R^2\) (Q887694) (← links)
• Error estimates of proper orthogonal decomposition eigenvectors and Galerkin projection for a general dynamical system arising in fluid models (Q938277) (← links)
• Averaging principle for quasi-geostrophic motion under rapidly oscillating forcing (Q939743) (← links)
• Trajectory attractor for the \(2d\) dissipative Euler equations and its relation to the Navier-Stokes system with vanishing viscosity (Q957810) (← links)
• Trajectory attractors for dissipative 2D Euler and Navier-Stokes equations (Q1033774) (← links)
• Time-periodic quasigeostrophic motion under dissipation and forcing (Q1294199) (← links)
• Dissipative quasi-geostrophic motion under temporally almost periodic forcing (Q1304608) (← links)
• Global well-posedness for the lake equations (Q1816834) (← links)
• Stratified models in geophysical fluid mechanics (Q1826252) (← links)
• Dynamics of quasi-geostrophic fluid motion with rapidly oscillating Coriolis force (Q1863665) (← links)
• Global well-posedness of the free-interface incompressible Euler equations with damping (Q1988302) (← links)
• Vanishing viscosity limit for global attractors for the damped Navier-Stokes system with stress free boundary conditions (Q1990068) (← links)
• An existence result for the steady rotating Prandtl equation (Q2219899) (← links)
• A weighted POD-reduction approach for parametrized PDE-constrained optimal control problems with random inputs and applications to environmental sciences (Q2239119) (← links)
• On the existence of almost-periodic solutions for the 2D dissipative Euler equations (Q2340467) (← links)
• Steady-state bifurcation analysis of a strong nonlinear atmospheric vorticity equation (Q2352170) (← links)
• A finite element discretization of the streamfunction formulation of the stationary quasi-geostrophic equations of the Ocean (Q2449943) (← links)
• Inviscid limit for damped and driven incompressible Navier-Stokes equations in \(\mathbb R^2\) (Q2472489) (← links)
• Regularity ``in large'' for the \(3D\) Salmon's planetary geostrophic model of ocean dynamics (Q2687509) (← links)
• FIXED-POINT ITERATION METHOD FOR NONLINEAR ROBUST CONTROL PROBLEMS IN FLUID MECHANICS (Q4806005) (← links)
• CHAOS IN WAVE INTERACTIONS (Q5297286) (← links)
• On the Euler equations of incompressible fluids (Q5446662) (← links)
• Continuous data assimilation of a discretized barotropic vorticity model of geophysical flow (Q6202627) (← links)
• Vanishing of long time average \(p\)-enstrophy dissipation rate in the inviscid limit of the 2D damped Navier-Stokes equations (Q6592102) (← links)