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Temperature regime and wind turbulence during formation of the low level jet streams in the stable boundary layer of atmosphere

The stable atmospheric boundary layer in the coastal zone of Lake Baikal was studied experimentally with a coherent Doppler wind lidar and a microwave temperature profiler. Two-dimensional height-time distributions of wind velocity components, temperature, and parameters characterizing the temperature conditions and wind turbulence have been obtained. Parameters of jet streams arising in the stable boundary layer have been determined. Variations of the Richardson number, dissipation rate of the kinetic energy of turbulence, variance of fluctuations of the radial velocity, and the outer scale of turbulence during the formation of jet streams in the boundary layer have been analyzed.