摘要
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
| 原文 | ???core.languages.en_GB??? |
|---|---|
| 頁(從 - 到) | 213-225 |
| 頁數 | 13 |
| 期刊 | Tellus, Series A |
| 卷 | 43 A |
| 發行號 | 3 |
| 出版狀態 | 已出版 - 1991 |