The primitive equations for the atmosphere and ocean, as well as its linearization, called the hydrostatic Stokes equation, are considered. The study of the latter problem in spaces of Lp- and anisotropic Lp-type yields results such as parabolic decay estimates as well as the property of maximal regularity. Applying these results to the full nonlinear problem yields the existence of unique global strong solutions to the primitive equations for a large class of initial data
Some new stable finite element (FE) schemes are presented for the hydrostatic Stokes system or prim...
Consider the primitive equations on R2 ×(z0, z1) with initial data a of the form a = a1 +a2, where a...
International audienceWe consider the linear Primitive Equations of the ocean in the three dimension...
The primitive equations for the atmosphere and ocean, as well as its linearization, called the hydro...
The primitive equations for the atmosphere and ocean, as well as its linearization, called the hydro...
The primitive equations for the atmosphere and ocean, as well as its linearization, called the hydro...
The primitive equations for the atmosphere and ocean, as well as its linearization, called the hydro...
In this work we will study, some types of regularity properties of solutions for the geophysical mod...
In 2016 Hieber and Kashiwabara showed that the three dimensional primitive equations admit a unique,...
Some new stable finite element (FE) schemes are presented for the hydrostatic Stokes system or prim...
Consider the 3-d primitive equations in a layer domain Ω = G×(−h,0), G = (0,1)2, subject to mixed Di...
In this thesis, we investigate the Stokes operator on bounded Lipschitz domains in L^p. We proof imp...
In this thesis, we investigate the Stokes operator on bounded Lipschitz domains in L^p. We proof imp...
In this thesis, we investigate the Stokes operator on bounded Lipschitz domains in L^p. We proof imp...
International audienceGlobal existence of weak and strong solutions to the quasi-hydrostatic primiti...
Some new stable finite element (FE) schemes are presented for the hydrostatic Stokes system or prim...
Consider the primitive equations on R2 ×(z0, z1) with initial data a of the form a = a1 +a2, where a...
International audienceWe consider the linear Primitive Equations of the ocean in the three dimension...
The primitive equations for the atmosphere and ocean, as well as its linearization, called the hydro...
The primitive equations for the atmosphere and ocean, as well as its linearization, called the hydro...
The primitive equations for the atmosphere and ocean, as well as its linearization, called the hydro...
The primitive equations for the atmosphere and ocean, as well as its linearization, called the hydro...
In this work we will study, some types of regularity properties of solutions for the geophysical mod...
In 2016 Hieber and Kashiwabara showed that the three dimensional primitive equations admit a unique,...
Some new stable finite element (FE) schemes are presented for the hydrostatic Stokes system or prim...
Consider the 3-d primitive equations in a layer domain Ω = G×(−h,0), G = (0,1)2, subject to mixed Di...
In this thesis, we investigate the Stokes operator on bounded Lipschitz domains in L^p. We proof imp...
In this thesis, we investigate the Stokes operator on bounded Lipschitz domains in L^p. We proof imp...
In this thesis, we investigate the Stokes operator on bounded Lipschitz domains in L^p. We proof imp...
International audienceGlobal existence of weak and strong solutions to the quasi-hydrostatic primiti...
Some new stable finite element (FE) schemes are presented for the hydrostatic Stokes system or prim...
Consider the primitive equations on R2 ×(z0, z1) with initial data a of the form a = a1 +a2, where a...
International audienceWe consider the linear Primitive Equations of the ocean in the three dimension...