| 海洋加热尺度对热带大气垂直环流圈结构的影响 |
| |
| 引用本文： | 巢纪平,王彰贵.海洋加热尺度对热带大气垂直环流圈结构的影响[J].南京气象学院学报,1991,14(1):10-17. |
| |
| 作者姓名： | 巢纪平 王彰贵 |
| |
| 作者单位： | 国家海洋环境预报研究中心
(巢纪平)，国家海洋环境预报研究中心(王彰贵) |
| |
| 摘 要： |
|
| 关 键 词： | 海洋 加热尺度 热带 大气 环流圈 |
INFLUENCE OF THE OCEAN HEATING SCALE ON THE STRUCTURE OF THE VERTICAL CIRCULATION CELL IN THE TROPICAL ATMOSPHERE |
| |
| Chao Jiping,Wang Zhanggui National Research Center for Marine Environment Forecasting.INFLUENCE OF THE OCEAN HEATING SCALE ON THE STRUCTURE OF THE VERTICAL CIRCULATION CELL IN THE TROPICAL ATMOSPHERE[J].Journal of Nanjing Institute of Meteorology,1991,14(1):10-17. |
| |
| Authors: | Chao Jiping Wang Zhanggui National Research Center for Marine Environment Forecasting |
| |
| Institution: | Chao Jiping;Wang Zhanggui National Research Center for Marine Environment Forecasting |
| |
| Abstract: | A steady, shallow water atmospheric model is used to studythe influence of the ocean heating scale on the structure of Walker andHad1ey circulation in the tropical atmosphere. It is shown that whenthe heating scale is smaller than the critical scale, the results are similarto Gill's (1980), that is,a hadley cell is located in the region of Rossbywaves and an anti-Hadley cell in the area of Kelvin waves. When theheating scale is larger than the critical scale. a Hadley cell exists inthe entire heating region. In the latter case, a large scale Hadley cellcan transfer a great amount of heat and energy from the ocean to theextratropical region. This causes the atmospheric circulation there tobe anomalous. The results are consistent with statistical facts and sup-port theoretically the teleconnection which Bjerknes put forward inthe 1960s. |
| |
| Keywords: | ocean heating scale tropical atmosphere vertical circulation cell |
| 本文献已被 CNKI 维普 等数据库收录！ |
