The strong solutions to the primitive equations coupled with multi-phase moisture atmosphere
From MaRDI portal
Publication:2083703
DOI10.1016/j.physd.2022.133442zbMath1496.86015OpenAlexW4285679638WikidataQ114180210 ScholiaQ114180210MaRDI QIDQ2083703
Publication date: 11 October 2022
Published in: Physica D (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1016/j.physd.2022.133442
Related Items (1)
Cites Work
- Unnamed Item
- Unnamed Item
- Unnamed Item
- Strong solutions to the 3D primitive equations with only horizontal dissipation: near \(H^{1}\) initial data
- Existence of the universal attractor for the 3-D viscous primitive equations of large-scale moist atmosphere
- The finite dimensional global attractor for the 3D viscous primitive equations
- Well-posedness of stochastic primitive equations with multiplicative noise in three dimensions
- 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.
- Global attractor of the three-dimensional primitive equations of large-scale Ocean and atmosphere dynamics
- On the effect of rotation on the life-span of analytic solutions to the \(3D\) Inviscid primitive equations
- Global well-posedness of stochastic 2D primitive equations with random initial conditions
- Global well-posedness of the 3D primitive equations with horizontal viscosity and vertical diffusivity
- On the effect of fast rotation and vertical viscosity on the lifespan of the \(3D\) Primitive equations
- On the well-posedness of reduced \(3D\) primitive geostrophic adjustment model with weak dissipation
- Phase transition models in atmospheric dynamics
- On the backward uniqueness of the stochastic primitive equations with additive noise
- The regularity of solutions of the primitive equations of the ocean in space dimension three
- The equations of the atmosphere with humidity and saturation: uniqueness and physical bounds
- Global well-posedness of the three-dimensional viscous primitive equations of large scale ocean and atmosphere dynamics
- Formulation of the equations of the humid atmosphere in the context of variational inequalities
- The global attractor for the solutions to the 3D viscous primitive equations
- The primitive equations approximation of the anisotropic horizontally viscous \(3D\) Navier-Stokes equations
- A tropical atmosphere model with moisture: global well-posedness and relaxation limit
- 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
- The equations of the multi-phase humid atmosphere expressed as a quasi variational inequality
- Global well-posedness for passively transported nonlinear moisture dynamics with phase changes
- Global well-posedness for the primitive equations coupled to nonlinear moisture dynamics with phase changes
- The primitive equations of the atmosphere in presence of vapour saturation
- RANDOM ATTRACTOR FOR THE 3D VISCOUS STOCHASTIC PRIMITIVE EQUATIONS WITH ADDITIVE NOISE
- On the regularity of the primitive equations of the ocean
This page was built for publication: The strong solutions to the primitive equations coupled with multi-phase moisture atmosphere