Published August 1, 2021 | Version v1
Journal article

Stability and optimal decay for a system of 3D anisotropic Boussinesq equations

  • 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 Ω = R 2 × T with T = [ 1 / 2 , 1 / 2 ] 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/ac08e9

Additional 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