【摘 要】
：
A three-layer theoretical model was established, in which the atmosphere is divided into three layers based on the Scorer parameter l2 , which is large in the m
【机 构】
：
Department of Martial Meteorology,State Key Laboratory of Atmospheric Sciences and Geophysical Fluid
【基金项目】
：
Opening Foundation of LASG and the National Natural Science Foundation of China
论文部分内容阅读
A three-layer theoretical model was established, in which the atmosphere is divided into three layers based on the Scorer parameter l2 , which is large in the middle layer and small in the other two layers. The wave number formula of lee waves was deduced with this theoretical model, and a typical example for the lee wave was calculated. Thus, the influence of changes in the thickness of every layer and values of the Scorer parameter in every layer was examined. The results show that the wavelength decreases with an increase in the thickness of the lower and the middle layers and is more sensitive to the changes in the middle layer. Therefore, if the changes in these two layers are different, the changes in the middle layer will dominate the changes in the wavelength. The results also show that the wavelength decreases with the increase in the value of l2 in every layer, among which the sensitivity to the l2 in the upper layer is the most striking. The calculation results reasonably can explain the influence of diurnal changes on the wavelength. The example was simulated using Advanced Regional Prediction System model, and the sensitivity experiments were performed to confirm the effects of the Scorer parameter profiles on the wavelengths. The simulated results are consistent with the calculated results.
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