Oscillations in the middle layer of a three-layer atmosphere induced by sources located in the lower layer are investigated. In every layer the Brunt-Vfiis~ilfi frequencies are constants and increase with height. The general solution obtained by the methods of integral transforms is presented in the
Resonance characteristics of linear lee waves in an atmosphere of three layers
β Scribed by F. H. Berkshire; A. O. Pickersgill
- Publisher
- John Wiley and Sons
- Year
- 1978
- Tongue
- English
- Weight
- 824 KB
- Volume
- 104
- Category
- Article
- ISSN
- 0035-9009
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β¦ Synopsis
Abstract
The upward leakage of wave energy from a twoβlayer troposphere into the stratosphere is examined; the changes produced in the natural complex modes of the system by altering the parameters are found to give rise to some quasiβresonance phenomena. Under special circumstances there may exist modes which decay extremely rapidly downstream and these provide a qualitative explanation for some features of observed flows.
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