Nonlinear stage of instability development in a stratified shear flow with an inflection-free velocity profile
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Publication:5304692
DOI10.1063/1.3159839zbMath1183.76152OpenAlexW1978130049MaRDI QIDQ5304692
Publication date: 18 March 2010
Published in: Physics of Fluids (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1063/1.3159839
Cites Work
- Unnamed Item
- On the weakly nonlinear three-dimensional instability of shear layers to pairs of oblique waves: the Stokes layer as a paradigm
- Stability analysis of stratified shear flows with a monotonic velocity profile without inflection points. Part 2. Continuous density variation
- Finite amplitude holmboe waves
- Considerations of the stability of certain heterogeneous shear flows including some inflexion-free profiles
- The nonlinear critical layer resulting from the spatial or temporal evolution of weakly unstable disturbances in shear flows
- Interaction of phase-locked modes: a new mechanism for the rapid growth of three-dimensional disturbances
- Effect of slight stratification on the nonlinear spatial evolution of a weakly unstable wave in a free shear layer
- Hydrodynamic Stability
- Nonlinear interactions between oblique instability waves on nearly parallel shear flows
- ON THE NONLINEAR EVOLUTION OF INSTABILITY MODES IN UNSTEADY SHEAR LAYERS: THE STOKES LAYER AS A PARADIGM
- The role of nonlinear critical layers in boundary layer transition
- Nonlinear stability of a stratified shear flow in the regime with an unsteady critical layer. Part 2. Arbitrary stratification of asymmetric flow
- Time-dependent critical layers in shear flows on the beta-plane
- On the catalytic role of the phase-locked interaction of Tollmien–Schlichting waves in boundary-layer transition
- Stability analysis of stratified shear flows with a monotonic velocity profile without inflection points
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