Pages that link to "Item:Q3796884"

The following pages link to Existence, uniqueness, and stability of stationary barotropic flow with forcing and dissipation (Q3796884):

Displaying 19 items.

• A two-level finite element discretization of the streamfunction formulation of the stationary quasi-geostrophic equations of the ocean (Q316202) (← links)
• Strong trajectory and global \(\mathbf{W^{1,p}}\)-attractors for the damped-driven Euler system in \(\mathbb R^2\) (Q520936) (← links)
• Upper bounds for the attractor dimension of damped Navier-Stokes equations in \(\mathbb R^2\) (Q887694) (← links)
• Multiplicity of time-periodic solutions and their stabilities for quasigeostrophic equations (Q1001247) (← links)
• Existence of solutions for three dimensional stationary incompressible Euler equations with nonvanishing vorticity (Q1047078) (← links)
• Time-periodic quasigeostrophic motion under dissipation and forcing (Q1294199) (← links)
• Baroclinic and barotropic aspects of the wind-driven ocean circulation (Q1600322) (← links)
• Analytic semigroup approach to generalized Navier-Stokes flows in Besov spaces (Q1690463) (← links)
• Vanishing viscosity limit for global attractors for the damped Navier-Stokes system with stress free boundary conditions (Q1990068) (← links)
• Hopf bifurcations and transitions of two-dimensional quasi-geostrophic flows (Q2032100) (← links)
• Steady-state bifurcation analysis of a strong nonlinear atmospheric vorticity equation (Q2352170) (← links)
• Hopf bifurcation and transition of three-dimensional wind-driven Ocean circulation problem (Q2416370) (← links)
• A finite element discretization of the streamfunction formulation of the stationary quasi-geostrophic equations of the Ocean (Q2449943) (← links)
• Existence of solutions for the barotropic-vorticity equation in an unbounded domain (Q2477814) (← links)
• Regularity ``in large'' for the \(3D\) Salmon's planetary geostrophic model of ocean dynamics (Q2687509) (← links)
• (Q3734082) (← links)
• Stability conditions and <i>a</i> <i>p</i> <i>r</i> <i>i</i> <i>o</i> <i>r</i> <i>i</i> estimates for equivalent-barotropic modons (Q3761923) (← links)
• Barotropic flow over finite isolated topography: steady solutions on the beta-plane and the initial value problem (Q4202230) (← links)
• Pseudo-advection method for the two-dimensional stationary Euler equations (Q4517479) (← links)