| Wang Zongshan,Xu Bochang,Jin Meibing,Zou Emei,Li Fanhua. 1998. A numerical prediction model of strong thermocline in the Bohai and the Huanghai Seas. Acta Oceanologica Sinica, (2):141－154 |
| A numerical prediction model of strong thermocline in the Bohai and the Huanghai Seas |
| A numerical prediction model of strong thermocline in the Bohai and the Huanghai Seas |
| Received:October 24, 1996 Revised:July 15, 1997 |
| DOI： |
| Key words:Three-dimensional numerical prediction strong thermocline |
| 中文关键词: Three-dimensional numerical prediction strong thermocline |
| 基金项目:This study was supported by the State Planning Commission. |
| Author Name | Affiliation | | Wang Zongshan | First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China | | Xu Bochang | First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China | | Jin Meibing | First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China | | Zou Emei | First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China | | Li Fanhua | First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China |
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| Abstract: |
| In this paper, the predecessors' research results of the numerical prediction models of vertical sea temperature structure calculation are reviewed and assessed, whereby a three-dimensional numerical prediction model of a strong thermocline is established by taking into account the absorbed and transmissive radiation at the sea surface, topography, wind stress, current speed, bottom friction and the mixing functions caused by them. As the driving elements of the model are only wind and air-temperature fields, the model has a fairly good practicality, and the results of trial prediction are satisfatory. |
| 中文摘要: |
| In this paper, the predecessors' research results of the numerical prediction models of vertical sea temperature structure calculation are reviewed and assessed, whereby a three-dimensional numerical prediction model of a strong thermocline is established by taking into account the absorbed and transmissive radiation at the sea surface, topography, wind stress, current speed, bottom friction and the mixing functions caused by them. As the driving elements of the model are only wind and air-temperature fields, the model has a fairly good practicality, and the results of trial prediction are satisfatory. |
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