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An equivalent depth of 10 m for the oscillations of the tropical atmosphere was suggested by wave-CISK calculations. It is here shown that the dispersive properties of such an atmosphere are in agreement with observed power spectra for southerly and westerly winds.
An equivalent depth of 10 m for the oscillations of the tropical atmosphere was suggested by wave-CISK calculations. It is here shown that the dispersive properties of such an atmosphere are in agreement with observed power spectra for southerly and westerly winds.
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| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 396 | 238 | 13 |
| PDF Downloads | 72 | 24 | 1 |
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