| A Further Inquiry on the Mechanism of 30-60 Day Oscillation in the Tropical Atmosphere |
| |
| 作者姓名： | Li Chongyin |
| |
| 摘 要： | In a simple semi-geostropic model on the equatorial β-plane, the theoretical analysis on the 30-60 day oscillation in the tropical atmosphere is further discussed based on the wave-CISK mechanism. The convection heat-ing can excite the CISK-Kelvin wave and CISK-Rossby wave in the tropical atmosphere and they are all the low-frequency modes which drive the activities of 30-60 day oscillation in the tropics. The most favorable conditions to excite the CISK-Kelvin wave and CISK-Rossby wave are indicated: There is convection heating but not very strong in the atmosphere and there is weaker disturbance in the lower troposphere.The influences of vertical shearing of basic flow in the troposphere on the 30-60 day oscillation in the tropics are also discussed.
|
A Further Inquiry on the Mechanism of 30-60 Day Oscillation in the Tropical Atmosphere |
| |
| Li Chongyin.A Further Inquiry on the Mechanism of 30-60 Day Oscillation in the Tropical Atmosphere[J].Advances in Atmospheric Sciences,1993,10(1):41-53. |
| |
| Authors: | Li Chongyin |
| |
| Institution: | LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100080 |
| |
| Abstract: | In a simple semi-geostropic model on the equatorialβ-plane, the theoretical analysis on the 30-60 day oscillation in the tropical atmosphere is further discussed based on the
wave-CISK mechanism. The convection heat-ing can excite the CISK-Kelvin wave and CISK-Rossby wave in the tropical atmosphere
and they are all the low-frequency modes which drive the activities of 30-60 day oscillation in the tropics. The most favorable
conditions to excite the CISK-Kelvin wave and CISK-Rossby wave are indicated: There is convection heating but not very strong
in the atmosphere and there is weaker disturbance in the lower troposphere.
The influences of vertical shearing of basic flow in the troposphere on the 30-60 day oscillation in the tropics are also
discussed. |
| |
| Keywords: | |
| 本文献已被 CNKI SpringerLink 等数据库收录！ |
| 点击此处可从《大气科学进展》浏览原始摘要信息 |
| 点击此处可从《大气科学进展》下载免费的PDF全文 |
