Stability and optimal decay for a system of 3D anisotropic Boussinesq equations
Creators
- 1. Department of Mathematics, Oklahoma State University, Stillwater, OK 74078 (United States)
- 2. Hebei Key Laboratory of Machine Learning and Computational Intelligence, School of Mathematics and Information Science, Hebei University, Baoding, 071002 (China)
Description
This paper focuses on a system of three-dimensional (3D) Boussinesq equations modeling anisotropic buoyancy-driven fluids. The goal here is to solve the stability and large-time behavior problem on perturbations near the hydrostatic balance, a prominent equilibrium in fluid dynamics, atmospherics and astrophysics. Due to the lack of the vertical kinematic dissipation and the horizontal thermal diffusion, this stability problem is difficult. When the spatial domain is with being a 1D periodic box, this paper establishes the desired stability for fluids with certain symmetries. The approach here is to distinguish the vertical averages of the velocity and temperature from their corresponding oscillation parts. In addition, the oscillation parts are shown to decay exponentially to zero in time. (paper)
Availability note (English)
Available from http://dx.doi.org/10.1088/1361-6544/ac08e9Additional details
Identifiers
Publishing Information
- Journal Title
- Nonlinearity (Print)
- Journal Volume
- 34
- Journal Issue
- 8
- Journal Page Range
- p. 5456-5484
- ISSN
- 0951-7715
INIS
- Country of Publication
- United Kingdom
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 53096015
- Subject category
- S71: CLASSICAL AND QUANTUM MECHANICS, GENERAL PHYSICS;
- Descriptors DEI
- ATMOSPHERICS; FLUID MECHANICS; FLUIDS; OSCILLATIONS; THERMAL DIFFUSION
- Descriptors DEC
- DIFFUSION; ELECTROMAGNETIC RADIATION; MECHANICS; NOISE; RADIATIONS; RADIO NOISE; RADIOWAVE RADIATION