Abstract
The structure of the intraseasonal oscillations in the tropics of an idealized general circulation model with a zonally symmetric climate is described. Space-time spectra show a peak in zonal winds and velocity potential at the equator in zonal wavenumbers 1 and 2, corresponding to eastward-propagating power at phase speeds of ≃18m s-1. This speed is significantly greater than that of the observed oscillation but comparable to that obtained in similar models by Hayashi and Sumi and Swinbank et al. The corresponding eastward-propagating power in the precipitation spectrum is concentrated in wavenumbers 2-5. A simple Kelvin wave-CISK model, in which the vertical structure of the heating is taken from the composite, is shown to be capable of reproducing the phase speed simulated in the GCM. -from Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 3810-3832 |
| Number of pages | 23 |
| Journal | Journal of the Atmospheric Sciences |
| Volume | 45 |
| Issue number | 24 |
| DOIs | |
| State | Published - 1988 |
| Externally published | Yes |
All Science Journal Classification (ASJC) codes
- Atmospheric Science
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