| NUMERICAL SIMULATION OF SEASONAL MOVEMENTS OF SUBTROPICAL HIGH RIDGE LINE Ⅱ.VAPOR CONDENSATION HEATING |
| |
| 引用本文： | 余志豪,葛孝贞.NUMERICAL SIMULATION OF SEASONAL MOVEMENTS OF SUBTROPICAL HIGH RIDGE LINE Ⅱ.VAPOR CONDENSATION HEATING[J].海洋学报(英文版),1986,5(2):183-194. |
| |
| 作者姓名： | 余志豪 葛孝贞 |
| |
| 作者单位： | Department of Meteorology, Nanjing University, Nanjing;Department of Meteorology, Nanjing University, Nanjing |
| |
| 摘 要： | The seasonal movement and jumping of subtropical high ridge line were simulated in the previous paper by using the two-dimensional zonal average model to consider the solar radiation heating. In this paper, the simulation is made by means of the same model considering water vapor condensation heating released from the rainfall belt north of subtropical high in addition to the solar radiation heating.The basic characteristics such as the northward seasonal jumping can still be simulated, and the condensation heating in the model can make the subtropical high ridge line move to the position a little further south than that without the condensation heating. Therefore, it may be realized that the basic characteristics of seasonal movement of subtropical high depend mainly on the solar radiation heating, but the meridional departure of ridge line from its normal latitude position is due to the feedback of drought-waterlogging in the precipitation area to the north of subtropical high.
|
| 收稿时间： | 1984/10/20 0:00:00 |
| 修稿时间： | 1985/7/12 0:00:00 |
NUMERICAL SIMULATION OF SEASONAL MOVEMENTS OF SUBTROPICAL HIGH RIDGE LINE Ⅱ.VAPOR CONDENSATION HEATING |
| |
| YU ZHIHAO and GE XIAOZHEN.NUMERICAL SIMULATION OF SEASONAL MOVEMENTS OF SUBTROPICAL HIGH RIDGE LINE Ⅱ.VAPOR CONDENSATION HEATING[J].Acta Oceanologica Sinica,1986,5(2):183-194. |
| |
| Authors: | YU ZHIHAO and GE XIAOZHEN |
| |
| Institution: | Department of Meteorology, Nanjing University, Nanjing |
| |
| Abstract: | The seasonal movement and jumping of subtropical high ridge line were simulated in the previous paper by using the two-dimensional zonal average model to consider the solar radiation heating.In this paper,the simulation is made by means of the same model considering water vapor condensation heating released from the rainfall belt north of subtropical high in addition to the solar radiation heating.The basic characteristics such as the northward seasonal jumping can still be simulated,and the condensation heating in the model can make the subtropical high ridge line move to the position a little further south than that without the condensation heating.Therefore,it may be realized that the basic characteristics of seasonal movement of subtropical high depend mainly on the solar radiation heating,but the meridional departure of ridge line from its normal latitude position is due to the feedback of drought-waterlogging in the precipitation area to the north of subtropical high. |
| |
| Keywords: | |
| 本文献已被 CNKI 等数据库收录！ |
| 点击此处可从《海洋学报(英文版)》浏览原始摘要信息 |
| 点击此处可从《海洋学报(英文版)》下载免费的PDF全文 |
