Averaging of the planetary 3D geostrophic equations with oscillating external forces
From MaRDI portal
Publication:434604
DOI10.1016/j.amc.2011.11.048zbMath1242.86010OpenAlexW2126760833MaRDI QIDQ434604
Publication date: 16 July 2012
Published in: Applied Mathematics and Computation (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1016/j.amc.2011.11.048
Related Items (1)
Cites Work
- Unnamed Item
- Unnamed Item
- Unnamed Item
- Unnamed Item
- Unnamed Item
- Unnamed Item
- Unnamed Item
- Unnamed Item
- Unnamed Item
- Unnamed Item
- Unnamed Item
- Non-autonomous planetary 3D geostrophic equations with oscillating external force and its global attractor
- A non-autonomous 3D Lagrangian averaged Navier-Stokes-\(\alpha\) model with oscillating external force and its global attractor
- Averaging of a 3D Lagrangian averaged Navier-Stokes-\(\alpha\) model with oscillating external forces
- Regularity results for linear elliptic problems related to the primitive equations.
- Attractors for 2D-Navier-Stokes models with delays
- Attractors for nonautonomous 2D Navier-Stokes equations with less regular normal forces
- Theorems about the attractor for incompressible non-Newtonian flow driven by external forces that are rapidly oscillating in time but have a smooth average
- Averaging of nonautonomous damped wave equations with singularly oscillating external forces
- Non-autonomous attractors for integro-differential evolution equations
- The existence and the structure of uniform global attractors for nonautonomous reaction-diffusion systems without uniqueness
- Infinite-dimensional dynamical systems in mechanics and physics
- Random attractors
- Nonautonomous systems, cocycle attractors and variable time-step discretization
- On mathematical problems for the primitive equations of the ocean: The mesoscale midlatitude case
- On non-autonomous sine-Gordon type equations with a simple global attractor and some averaging
- Asymptotic analysis of the primitive equations under the small depth assumption
- The primitive equations on the large scale ocean under the small depth hypothesis.
- Mathematical theory for the coupled atmosphere-ocean models (CAO III)
- Non-autonomous 2D Navier-Stokes system with singularly oscillating external force and its global attractor
- Global well-posedness of the three-dimensional viscous primitive equations of large scale ocean and atmosphere dynamics
- Attractors for nonautonomous 2D Navier-Stokes equations with normal external forces
- The global attractor for the solutions to the 3D viscous primitive equations
- Averaging of trajectory attractors of evolution equations with rapidly oscillating terms
- Asymptotic behaviour of two–dimensional Navier–Stokes equations with delays
- On the existence of pullback attractors for non-autonomous reaction–diffusion equations
- Averaging of 2D Navier–Stokes equations with singularly oscillating forces
- Attractors of non-autonomous reaction–diffusion equations
- New formulations of the primitive equations of atmosphere and applications
- On the equations of the large-scale ocean
- Barotropic-Baroclinic Formulation of the Primitive Equations of the Ocean
- Some mathematical properties of the planetary geostrophic equations for large-scale ocean circulation
- Global well‐posedness and finite‐dimensional global attractor for a 3‐D planetary geostrophic viscous model
This page was built for publication: Averaging of the planetary 3D geostrophic equations with oscillating external forces