Abstract:The paper presents the results of studies of atmospheric turbulence in the lower part of the atmospheric boundary layer. At different heights of the atmosphere (8, 121, 301 m), the energetic loses of air flow for the generation of turbulent kinetic energy are calculated for different linear scales. It is shown that on small scales the consumption of mean kinetic energy to energy of turbulence reaches 32% in winter (at 8 m) and 34% (at 301 m) in summer. The paper also uses the WRF model, for the first time in R… Show more
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