A note on the asymptotic interpretation of the classical theory of lee waves in the troposphere and the role of the upper boundary condition

DOI10.1080/03091927908242677zbMath0441.76016OpenAlexW2145101041WikidataQ114640904 ScholiaQ114640904MaRDI QIDQ3883772

J.-P. Guiraud, Radyadour Kh. Zeytounian

Publication date: 1979

Published in: Geophysical & Astrophysical Fluid Dynamics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1080/03091927908242677

zbMATH Keywords

perturbationstroposphereinviscid perfect gasnonlinear motionupper boundary conditionLong's equationasymptotic interpretationlee wavesMiles' model

Mathematics Subject Classification ID

Geophysics (86A99)

Related Items (2)

Asymptotic theory of lee waves in an unbounded atmosphere ⋮ Recent advances in asymptotic modelling of tangent atmospheric motions

Cites Work

• Spherical means and radiation conditions
• Effect of viscosity on gravity waves and the upper boundary condition
• Lee waves in a stratified flow Part 3. Semi-elliptical obstacle
• Finite amplitude instability of second-order fluids in plane Poiseuille flow
• A similarity solution for viscous internal waves
• Theorie der stationären Leewellenströmung in freier Atmosphäre
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