## Abstract During a routine instrumentation flight check in the lower stratosphere periodic variations of temperature and winds were observed. It is deduced that these variations are gravity waves which appear to be associated with a narrow frontal zone separating regions with different potential
โฆ LIBER โฆ
Observed generation of an atmospheric gravity wave by shear instability in the mean flow of the planetary boundary layer
โ Scribed by W. H. Hooke; F. F. Hall; E. E. Gossard
- Publisher
- Springer
- Year
- 1973
- Tongue
- English
- Weight
- 954 KB
- Volume
- 5
- Category
- Article
- ISSN
- 0006-8314
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