The results show that the intensity of the angle-of-arrival fluctuation in the haze weather and low visibility is smaller than that in the clear-air weather and high visibility.
英
美
释义
在强湍流区,到达角起伏出现饱和效应,在弱湍流区,到达角起伏的强度随着湍流强度的增加而增强;
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