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A quasi-three-dimensional numerical prediction model of salinity structure in Bohai Sea and Huanghai Sea

A quasi-three-dimensional numerical prediction model of salinity structure in Bohai Sea and Huanghai Sea
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摘要 The vertical salinity structure in the Bohai As and the Huanghai Sea have typical self-similar characters. However, horizontal salinity distribution is influenced by advection, horizontal diffusion, river discharge,etc. By using observed sea salinity data, a similarity function of vertical salinity profiles of the Bohai Sea and the Huanghai Sea has been constructed. On the basis of vertical integrated equations of motion and equation of continuity, and governing equations about the distribution of 3 characteristic factors (surface salinity Ss, bottom salinity SH, and thickness of upper homogeneous layer h), and combined with the similarity function, a quasithree-dimensional numerical model of salinity structure bas ben developed. In the model, the comprehensive effects of sea surface wind stress and heat influx, advection, diffusion, entrainment, bottom as well as lateral eddy mixture are taken into consideration. It is shown that the numerical model is more practical and the results of the trial prediction are satisfactory The vertical salinity structure in the Bohai As and the Huanghai Sea have typical self-similar characters. However, horizontal salinity distribution is influenced by advection, horizontal diffusion, river discharge,etc. By using observed sea salinity data, a similarity function of vertical salinity profiles of the Bohai Sea and the Huanghai Sea has been constructed. On the basis of vertical integrated equations of motion and equation of continuity, and governing equations about the distribution of 3 characteristic factors (surface salinity Ss, bottom salinity SH, and thickness of upper homogeneous layer h), and combined with the similarity function, a quasithree-dimensional numerical model of salinity structure bas ben developed. In the model, the comprehensive effects of sea surface wind stress and heat influx, advection, diffusion, entrainment, bottom as well as lateral eddy mixture are taken into consideration. It is shown that the numerical model is more practical and the results of the trial prediction are satisfactory
出处 《Acta Oceanologica Sinica》 SCIE CAS CSCD 1994年第4期485-494,共10页 海洋学报(英文版)
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