Pages that link to "Item:Q3306591"

The following pages link to Continuous dependence on boundary parameters for three-dimensional viscous primitive equation of large-scale ocean atmospheric dynamics (Q3306591):

Displaying 9 items.

• Continuous dependence of 2D large scale primitive equations on the boundary conditions in oceanic dynamics. (Q2076582) (← links)
• Convergence results on the boundary conditions for 2D large-scale primitive equations in oceanic dynamics (Q2195494) (← links)
• Continuous dependence on viscosity coefficient for primitive equations (Q3308078) (← links)
• Continuous dependence of primitive equations of the atmosphere with vapor saturation (Q3381096) (← links)
• The continuous dependence of three-dimensional primitive equations with heat and salinity diffusion (Q3381146) (← links)
• Continuous dependence of primitive equations of large-scale moist atmosphere on viscosity coefficient (Q3385896) (← links)
• The applications of some basic mathematical inequalities on the convergence of the primitive equations of moist atmosphere (Q4992483) (← links)
• (Q5143732) (← links)
• Structural stability for the Brinkman-Forchheimer equations interfacing with a Darcy equations (Q6654090) (← links)