Existence of a strong solution and trajectory attractor for a climate dynamics model with topography effects
From MaRDI portal
Publication:1674416
DOI10.1016/j.jmaa.2017.09.025zbMath1375.35561OpenAlexW2754466394MaRDI QIDQ1674416
Publication date: 2 November 2017
Published in: Journal of Mathematical Analysis and Applications (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1016/j.jmaa.2017.09.025
Attractors (35B41) Hydrology, hydrography, oceanography (86A05) Dynamical systems in biology (37N25) Meteorology and atmospheric physics (86A10) PDEs in connection with geophysics (35Q86) Strong solutions to PDEs (35D35)
Related Items (7)
Local well-posedness of strong solution to a climate dynamic model with phase transformation of water vapor ⋮ Existence of a strong solution to moist atmospheric equations with the effects of topography ⋮ The primitive equations approximation of the anisotropic horizontally viscous \(3D\) Navier-Stokes equations ⋮ Global existence and asymptotic stability of the free boundary problem of the primitive equations with heat insulation ⋮ Blow-up criterion of solutions of the horizontal viscous primitive equations with horizontal eddy diffusivity ⋮ An overview of the dynamic framework in earth-system model and its well-posedness ⋮ Global existence of the strong solution to the climate dynamics model with topography effects and phase transformation of water vapor
Cites Work
- Existence of the universal attractor for the 3-D viscous primitive equations of large-scale moist atmosphere
- Local and global well-posedness of strong solutions to the 3D primitive equations with vertical Eddy diffusivity
- Global well-posedness of strong solutions to the 3D primitive equations with horizontal eddy diffusivity
- Global well-posedness of the \(3D\) primitive equations with partial vertical turbulence mixing heat diffusion
- Infinite-dimensional dynamical systems in mechanics and physics.
- Anisotropic estimates and strong solutions of the primitive equations.
- Mathematical theory for the coupled atmosphere-ocean models (CAO III)
- Global well-posedness of the 3D primitive equations with horizontal viscosity and vertical diffusivity
- Stability of weak solutions for the large-scale atmospheric equations
- Global well-posedness of the three-dimensional viscous primitive equations of large scale ocean and atmosphere dynamics
- Global Well-Posedness of the Three-Dimensional Primitive Equations with Only Horizontal Viscosity and Diffusion
- Existence of weak solutions and trajectory attractors for the moist atmospheric equations in geophysics
- New formulations of the primitive equations of atmosphere and applications
- A horizontal hyper-diffusion three-dimensional thermocline planetary geostrophic model: well-posedness and long-time behaviour
- Global well‐posedness and finite‐dimensional global attractor for a 3‐D planetary geostrophic viscous model
- Weak solutions to a model of climate dynamics
- Unnamed Item
- Unnamed Item
- Unnamed Item
- Unnamed Item
- Unnamed Item
This page was built for publication: Existence of a strong solution and trajectory attractor for a climate dynamics model with topography effects
