Abstract
It was found that the jet possesses a distinctive intraseasonal oscillation south of its core. Previous studies suggested that the temporal fluctuation of this jet may be related through cumulus convection to that of the low-level Indian monsoon circulation. It was demonstrated by a streamfunction budget analysis that the intraseasonal oscillation of the tropical easterly jet south of its core is primarily induced by the eastward-propagating intraseasonal oscillation of the planetary-scale divergent circulation. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 213-225 |
| Number of pages | 13 |
| Journal | Tellus, Series A |
| Volume | 43 A |
| Issue number | 3 |
| State | Published - 1991 |