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Lidar studies of fluctuation spectra of the coefficient of backscattering in atmospheric surface layer

机译:大气表面层后向散射系数波动谱的激光雷达研究

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Abstract: In this paper we present experimental data of studies of fluctuation spectra of the backscattering coefficient by the synchronous registration of three components of wind velocity, temperature and backscattering coefficient in the local air volume at height equal to 5 meter. Measurements were carried out by means of the acoustic meteostation and with the aerosol laser locator. Obtained results had verified differences between of power auto-spectra of wind velocity fluctuations and backscattering coefficient fluctuations at stable thermal stratification, presumably explained away as the effects of temperature stratification and of convective turbulence. When stratification of the surface layer is stable there appears a 'sub- area of buoyancy' (the Boljiano-Monin spectrum) in fluctuation spectra of the coefficient of backscattering. Assuming that the field of concentration of particles is formed at upper boundary of the boundary layer, and then it without substantial changes it delivers by downgoing flows to the earth surface. !19
机译:摘要:本文介绍了通过同步记录风速,温度和后向散射系数三个分量在高度等于5米的局部风中对后向散射系数的波动谱进行研究的实验数据。通过声学流变仪和气溶胶激光定位仪进行测量。所得结果证实了在稳定的热分层情况下风速波动的功率自谱与反向散射系数波动之间的差异,大概可以解释为温度分层和对流湍流的影响。当表层的分层稳定后,在反向散射系数的波动谱中会出现一个“浮力子区域”(Boljiano-Monin谱)。假设在边界层的上边界处形成了粒子的浓度场,然后在没有实质性变化的情况下,它通过向下流向地表的方式传递。 !19

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