[HTML][HTML] Strichartz estimates for the Euler equations in the rotational framework
Y Koh, S Lee, R Takada - Journal of Differential Equations, 2014 - Elsevier
We consider the initial value problems of the incompressible Euler equations in the
rotational framework. We obtain the optimal range of the Strichartz estimate for the linear …
rotational framework. We obtain the optimal range of the Strichartz estimate for the linear …
Sharp well-posedness and ill-posedness of the three-dimensional primitive equations of geophysics in Fourier–Besov spaces
J Sun, S Cui - Nonlinear Analysis: Real World Applications, 2019 - Elsevier
We study the well-posedness and ill-posedness for the Cauchy problem of the three-
dimensional primitive equations describing the large-scale oceanic and atmospheric …
dimensional primitive equations describing the large-scale oceanic and atmospheric …
Global solutions for the incompressible rotating stably stratified fluids
T Iwabuchi, A Mahalov, R Takada - Mathematische …, 2017 - Wiley Online Library
We consider the initial value problem of the 3D incompressible Boussinesq equations for
rotating stratified fluids. We establish the dispersive and the Strichartz estimates for the …
rotating stratified fluids. We establish the dispersive and the Strichartz estimates for the …
Global existence for the primitive equations with small anisotropic viscosity
F Charve, VS Ngo - 2011 - ems.press
In this paper, we consider the primitive equations with zero vertical viscosity, zero vertical
thermal diffusivity, and the horizontal viscosity and horizontal thermal diffusivity of size εα …
thermal diffusivity, and the horizontal viscosity and horizontal thermal diffusivity of size εα …
Global well-posedness for the fractional Boussinesq–Coriolis system with stratification in a framework of Fourier–Besov type
We establish the global well-posedness of the 3D fractional Boussinesq–Coriolis system
with stratification in a framework of Fourier type, namely spaces of Fourier–Besov type with …
with stratification in a framework of Fourier type, namely spaces of Fourier–Besov type with …
Multi-scale methods for geophysical flows
Geophysical flows comprise a broad range of spatial and temporal scales, from planetary-to
meso-scale and microscopic turbulence regimes. The relation of scales and flow …
meso-scale and microscopic turbulence regimes. The relation of scales and flow …
Asymptotics and lower bound for the lifespan of solutions to the Primitive Equations
F Charve - Acta Applicandae Mathematicae, 2018 - Springer
In a previous work we obtained a large lower bound for the lifespan of the solutions to the
Primitive Equations, and proved convergence to the 3D quasi-geostrophic system for …
Primitive Equations, and proved convergence to the 3D quasi-geostrophic system for …
Global well-posedness for the primitive equations with less regular initial data
F Charve - Annales de la Faculté des sciences de Toulouse …, 2008 - numdam.org
This paper is devoted to the study of the lifespan of the solutions of the primitive equations
for less regular initial data. We interpolate the globall well-posedness results for small initial …
for less regular initial data. We interpolate the globall well-posedness results for small initial …
Asymptotics for the rotating fluids and primitive systems with large ill-prepared initial data in critical spaces
F Charve - Tunisian Journal of Mathematics, 2023 - msp.org
We study the lifespan and asymptotics (in the large rotation and stratification regime) for the
primitive system for highly ill-prepared initial data in critical spaces. Compared to our …
primitive system for highly ill-prepared initial data in critical spaces. Compared to our …
Long time existence of classical solutions for the 3D incompressible rotating Euler equations
R Takada - Journal of the Mathematical Society of Japan, 2016 - jstage.jst.go.jp
We consider the initial value problem of the 3D incompressible rotating Euler equations. We
prove the long time existence of classical solutions for initial data in Hs (R3) with s> 5/2 …
prove the long time existence of classical solutions for initial data in Hs (R3) with s> 5/2 …