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Determination of turbulent-layer wind speed from G-SCIDAR data using an algorithm based on wavelet transforms

机译:基于小波变换的算法,从G-SCIDAR数据确定湍流层风速

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The determination of turbulent-layers wind speed observed through Generalized SCIDAR technique (G-SCIDAR) requires an efficient and contrasted code. We have developed a fully automated algorithm based on wavelet transforms to derive the velocity magnitude and direction of atmospheric turbulent layers from G-SCIDAR measurements. The algorithm makes use of five cross-correlations of a series of scintillation patterns separated by lapses of Δt, 2Δt, 3Δt, 4Δt and 5Δt. The wavelet analysis of such cross-correlation images provides the position, direction and altitude of the different turbulent layers detected in each image. The comparison and consistency of results in consecutive cross-correlations allows the determination of the turbulence layers velocities and avoids misidentifications associated with noise and/or overlapping layers. The software includes the correction due to the projection effects on the observing direction of the actual velocity vector of turbulence layers. The algorithm has been applied to simulated data with excellent results, as well as to actual G-SCIDAR observations. For the validation of velocities derived for real G-SCIDAR data we have compared them to the velocities provided by balloon measurements. The software has been designed to analyze huge amounts of G-SCIDAR measurements.
机译:通过广义的SCIDAR技术(G-SCIDAR)观察到湍流层风速需要有效和对比的代码。我们已经开发了一种基于小波变换的全自动算法,从G-SCIDAR测量导出大气湍流层的速度幅度和方向。该算法利用由ΔT,2ΔT,3ΔT,4ΔT和5ΔT分开的一系列闪烁图案的五个横相关。这种互相关图像的小波分析提供了在每个图像中检测到的不同湍流层的位置,方向和高度。连续交叉相关结果的比较和一致性允许确定湍流层速度并避免与噪声和/或重叠层相关的误识别。该软件包括由于对湍流层的实际速度矢量的观察方向的投影效应引起的校正。该算法已应用于具有优异结果的模拟数据,以及实际的G-SCIDAR观察。为了验证用于真实G-SCIDAR数据的速度,我们已经将它们与气球测量提供的速度进行了比较。该软件旨在分析大量G-SCIDAR测量。

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