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Remote sensing of humidity fluctuations in the atmosphere

机译:遥感大气中的湿度波动

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Abstract: The structure constant of humidity fluctuations is an important statistical characteristic of the turbulent atmosphere. We propose a new method for the remote sensing of this structure constant using bistatic acoustic sounding. First of all, the new approximate equation for a sound wave in a turbulent medium with random inhomogeneities of the adiabatic sound speed, density and medium velocity is presented. This equation has a wider range of applicability than equations used before in the theory of sound propagation in turbulent media. Starting from this equation, the sound scattering cross-section $sigma in the turbulent atmosphere is calculated. From the obtained equation it follows that at the scattering angle $theta $EQ 90$DGR the sound wave is scattered only by humidity fluctuations. Therefore, measuring the scattering cross-section $sigma@(90$DGR@) by bistatic acoustic sounding we can obtain the structure constant of humidity fluctuations in the atmosphere. Some problems of practical realization of the proposed method are considered. !11
机译:摘要:湿度波动的结构常数是湍流大气的重要统计特征。我们提出了一种利用双基地声测深遥感这种结构常数的新方法。首先,给出了具有绝热声速,密度和介质速度的随机不均匀性的湍流介质中声波的新近似方程。该方程比在湍流介质中的声音传播理论中以前使用的方程具有更大的适用范围。从该方程式开始,计算了湍流大气中的声散射截面$ sigma。从获得的方程式可以得出,在散射角$ theta $ EQ 90 $ DGR时,声波仅因湿度波动而散射。因此,通过双基地声测得散射截面$ sigma @(90 $ DGR @),我们可以得到大气湿度波动的结构常数。考虑了该方法实际实现的一些问题。 !11

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