| A study on the numerical prediction method for the vertical thermal structure in the Bohai Sea and the Huanghai Sea-Ⅰ. One-dimensional numerical prediction model |
| |
| 作者姓名： | Wang Zongshan Xu Bochang Zou Emei Yang Keqi Li Fanhua |
| |
| 作者单位： | First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China;First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China;First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China;First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China;First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China |
| |
| 摘 要： | In this paper,on the basis of the heat conduction equation without consideration of the advection and turbulence effects,one-dimensional model for describing surface sea temperature (Ts),bottom sea temperature (Th) and the thickness of the upper homogeneous layer (h) is developed in terms of the dimensionless temperature θT and depth η and self-simulation function θT-f(η) of vertical temperature profile by means of historical temperature data.The results of trial prediction with our one-dimensional model on Ts,Th,h,the thickness and gradient of thermocline are satisfactory to some extent.
|
| 收稿时间： | 1989/10/20 0:00:00 |
| 修稿时间： | 1990/4/10 0:00:00 |
A study on the numerical prediction method for the vertical thermal structure in the Bohai Sea and the Huanghai Sea-Ⅰ. One-dimensional numerical prediction model |
| |
| Wang Zongshan,Xu Bochang,Zou Emei,Yang Keqi,Li Fanhua.A study on the numerical prediction method for the vertical thermal structure in the Bohai Sea and the Huanghai Sea-Ⅰ. One-dimensional numerical prediction model[J].Acta Oceanologica Sinica,1992,11(1):25-34. |
| |
| Authors: | Wang Zongshan Xu Bochang Zou Emei Yang Keqi and Li Fanhua |
| |
| Institution: | First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China |
| |
| Abstract: | In this paper,on the basis of the heat conduction equation without consideration of the advection and turbulence effects,one-dimensional model for describing surface sea temperature (Ts),bottom sea temperature (Th) and the thickness of the upper homogeneous layer (h) is developed in terms of the dimensionless temperature θT and depth η and self-simulation function θT-f(η) of vertical temperature profile by means of historical temperature data.
The results of trial prediction with our one-dimensional model on Ts,Th,h,the thickness and gradient of thermocline are satisfactory to some extent. |
| |
| Keywords: | |
|
| 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 |
|
