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Wang Xiuqin,Huang Huowang,Deng Jian,Qian Chengchun. 2001. Test of numerical prediction of sea water temperature in the Taiwan Strait. Acta Oceanologica Sinica, (4):473-481
Test of numerical prediction of sea water temperature in the Taiwan Strait
Test of numerical prediction of sea water temperature in the Taiwan Strait
Received:July 25, 2001  Revised:August 08, 2001
DOI:
Key words:The Taiwan Strait  numerical prediction of sea water temperature
中文关键词:  The Taiwan Strait  numerical prediction of sea water temperature
基金项目:The project was financially supported by the Natural Science Foundation of Province under contract No. Q99E02 and the special fund for authors excellent Ph. D. Dissertation of the whole country under contract No.200021.
Author NameAffiliation
Wang Xiuqin Department of Oceanography, Ocean University of Qingdao, Qingdao 266003, China 
Huang Huowang Marine Prediction Stage of Xiamen, Xiamen 361002, China 
Deng Jian Marine Prediction Stage of Xiamen, Xiamen 361002, China 
Qian Chengchun Department of Oceanography, Ocean University of Qingdao, Qingdao 266003, China 
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Abstract:
      A dynamic numerical prediction model of sea water temperature for limited sea area is used to predict the sea water temperature at the sea area near Fujian. Essential adjustments have been made in accordance with the characteristics of this region. Two tests have been made. One is in summer (3 d) and the other is in winter (10 d). In the summer test, a typhoon is just passing by and the calculated current field well responds to typhoon. In the winter test, variation tendency of the predicted sea water temperature field agrees with that of the observation basically, the absolute mean error in the whole sea area is 0.6℃. The variation of the sea water temperature is mostly affected by entrainment and pumping, which is related to the topography of the strait.
中文摘要:
      A dynamic numerical prediction model of sea water temperature for limited sea area is used to predict the sea water temperature at the sea area near Fujian. Essential adjustments have been made in accordance with the characteristics of this region. Two tests have been made. One is in summer (3 d) and the other is in winter (10 d). In the summer test, a typhoon is just passing by and the calculated current field well responds to typhoon. In the winter test, variation tendency of the predicted sea water temperature field agrees with that of the observation basically, the absolute mean error in the whole sea area is 0.6℃. The variation of the sea water temperature is mostly affected by entrainment and pumping, which is related to the topography of the strait.
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