Published February 2005 | Version v1
Journal article

Stability of stratified flow with inhomogeneous shear

  • 1. Kharkov National University, 61108 Kharkov (Ukraine)
  • 2. Physics Department, West Virginia University, Morgantown, West Virginia, 26506 (United States)
  • 3. Kharkov National University, 61108 Kharkov, Ukraine and National Science Center 'Kharkov Institute of Physics and Technology', Scientific and Production Complex 'Renewable energy sources and sustainable technologies', 61108 Kharkov (Ukraine)

Description

The temporal evolution of perturbations in stratified flow with inhomogeneous shear is examined analytically by an extension of the nonmodal approach to flows with inhomogeneous shear. The solutions of the equations that govern the linear evolution and the weak nonlinear evolution of perturbations of the stream function for stratified flow with monotonic inhomogeneous shear are obtained. It is shown that stabilization of perturbations arises from nonmodal effects due to flow shear. Conditions at which these nonmodal effects may be strong enough to stabilize the Rayleigh-Taylor instability are presented. These analytical results are also compared to numerical simulations of the governing equations performed by Benilov, Naulin, and Rasmussen

Additional details

Identifiers

Publishing Information

Journal Title
Physical Review. E, Statistical Physics, Plasmas, Fluids, and Related Interdisciplinary Topics
Journal Volume
71
Journal Issue
2
Journal Page Range
p. 026306-026306.8
ISSN
1063-651X
CODEN
PLEEE8

INIS

Country of Publication
United States
Country of Input or Organization
International Atomic Energy Agency (IAEA)
INIS RN
36083284
Subject category
S71: CLASSICAL AND QUANTUM MECHANICS, GENERAL PHYSICS; S70: PLASMA PHYSICS AND FUSION TECHNOLOGY;
Descriptors DEI
EQUATIONS; FLUID FLOW; FUNCTIONS; MATHEMATICAL EVOLUTION; MATHEMATICAL SOLUTIONS; NONLINEAR PROBLEMS; PERTURBATION THEORY; RAYLEIGH-TAYLOR INSTABILITY; SHEAR; SIMULATION; STABILITY; STABILIZATION
Descriptors DEC
EVOLUTION; INSTABILITY

Optional Information

Notes
(c) 2005 The American Physical Society