Critical-level crossing of rossby-gravity wave-packets in a linear-shear, stratified flow
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Publication:3741262
DOI10.1080/03091928608245887zbMath0604.76017OpenAlexW2019282612WikidataQ114640387 ScholiaQ114640387MaRDI QIDQ3741262
Publication date: 1986
Published in: Geophysical & Astrophysical Fluid Dynamics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1080/03091928608245887
existencecontinuous spectrumhypergeometric functionswave packetsanalytic solutionsbounded systemslinear shear flowdiscrete point eigenvalueregular normal modesRossby-gravity waves
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Cites Work
- The special functions and their approximations. Vol. I, II
- Stability of an Idealized Atmosphere. I. Discussion of Results
- Stability of an Idealized Atmosphere. II. Zeros of the Confluent Hypergeometric Function
- The continuous spectrum in differentially rotating perfect fluids: a model with an analytic solution
- Perturbations of Plane Couette Flow in Stratified Fluid and Origin of Cloud Streets
- Wave propagation in a stratified shear flow
- Effect of variation in density on the stability of superposed streams of Fluid
- The critical layer for internal gravity waves in a shear flow
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