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本文将相似理论应用于暖季混合层(温跃层)深度的预报。假设作用过程是非平流和非扩散的。所使用的参数是风、科氏参数、热膨胀系数和混合层内的热储量,在预报模式中应用了Kitaigorodsii的普遍函数概念。最终的预报模式主要包括两个方程,方程中的系数是由1975-1981年暖季东海的实测资料确定的。在东海的两个特点海域中进行的试验证明预报模式具有较好的适应性。
This paper applies the theory of similarity to the prediction of the depth of the warm season mixed layer (thermocline). Suppose the course of action is non-advection and non-proliferation. The parameters used are the wind, the Coriolis parameters, the thermal expansion coefficient and the heat storage in the mixed layer, and the universal function concept of Kitaigorodsii is applied in the prediction mode. The final forecasting model mainly includes two equations. The coefficients in the equation are determined from the measured data of the East China Sea during the warm season of 1975-1981. Experiments conducted in the two sea areas of the East China Sea proved that the prediction model has a good adaptability.