In this paper, a method is proposed to estimate wind turbulence parameters using\nmeasurements recorded by a conically scanning coherent Doppler lidar with two different elevation\nangles. This methodology helps determine the anisotropy of the spatial correlation of wind velocity\nturbulent fluctuations. The proposed method was tested in a field experiment with a Stream Line\nlidar (Halo Photonics, Brockamin, Worcester, United Kingdom) under stable temperature\nstratification conditions in the atmospheric boundary layer. The results show that the studied\nanisotropy coefficient in a stable boundary layer may be up to three or larger.
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