## Abstract It is demonstrated that diurnal and semiβdiurnal variations of wind occur in the lower stratosphere. These oscillations appear to be associated with the solar tides. The stratospheric semiβdiurnal oscillation of wind is in phase with, and of comparable magnitude to, the surface semiβdiu
β¦ LIBER β¦
Tidal oscillations of the lower stratosphere
β Scribed by D. H. Johnson
- Publisher
- John Wiley and Sons
- Year
- 1955
- Tongue
- English
- Weight
- 74 KB
- Volume
- 81
- Category
- Article
- ISSN
- 0035-9009
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