Ll 23:00 to receive 10 min averages and to exclude outliers. Formulas for calculating EMKE (r, t) and ETKE (r, t) are presented in [10]. Final results of calculations of the diurnal hourly dynamics on the wind velocity vector, relative contributions of the mean and turbulent elements in the wind kinetic energy, and also the kinetic power flux density vector in the information of continuous 24-h minisodar measurements are presented under. The raw minisodar information series have been sampled just about every hour from 00:00 till 23:00, local time. Series of N = 150 vertical profiles in the wind vector components have been processed, which offered data averaging more than 10 min periods. Statistical evaluation of the final results of minisodar measurements of vertical profiles of wind velocity elements in the 500 m layer in the atmosphere performed in [12] showed that this problem belongs for the class of robust nonparametric troubles of mathematical statistics. The raw minisodar information series had been preprocessed to exclude outliers working with the consecutive nonparametric approach of adaptive pendular truncation for outlier detection developed by us and implemented within the censoring algorithm described in detail in [13]. The confidence intervals had been discovered employing bootstrap. It was demonstrated that the variances on the wind vector elements decreased by two.50 times based on the sounding altitude. These studies demonstrated the efficiency of your proposed algorithm. Working with the algorithm of pendular truncation, outliers of a variety of origins have been excluded in the samples, as well as the truncated estimates of your wind vector components and their variances have been then processed. four. Outcomes and Discussion The diurnal hourly dynamics from the wind velocity vector, the relative contributions with the mean and turbulent kinetic energy elements, and also the total kinetic flux power density vector are presented beneath. 4.1. Diurnal Hourly Dynamics of your Wind Velocity Vector Figure 1 shows the diurnal hourly dynamics with the wind velocity vector retrieved from minisodar measurements with 10-min averaging. The observations began at ten:00, regional time, and completed at 24:00. Here, the length with the vector shows its magnitude, northern direction is upward, southern is downward, east would be to the proper, and west is always to the left. It may be observed that irrespective from the observation time, the wind direction at altitudes up to one hundred m undergoes no sharp adjustments with increasing altitude. At altitudes from 100 m to 200 m, the wind path undergoes perturbations; moreover, if at ten:00 perturbationsAtmosphere 2021, 12,till 17:00, the wind velocity vectors considerably exceeded their corresponding ��-cedrene medchemexpress evening values (from 18:00 till 23:00), and a lowlevel jet was observed the maximum of which increased from 25 m at ten:00 to 75 m at 15:00. Our evaluation of your diurnal hourly dynamics of your x, y, and z wind vector compo nents demonstrated that in the daytime, maximum values with the horizontal elements four of 11 had been observed from ten:00 till 16:007:00. The minimal values on the horizontal compo nents have been observed late inside the evening from 20:00 till 23:00. It is critical that at altitudes up to 5000 m, the wind velocity vector didn’t expertise sharp changes with rising began from 150 m, at 14:00, they started currently from 200 m. The decrease horizon from the altitude and smoothly changed using the time with the day. At any time, maximal perturba layer of enhanced turbulence descended from 16:00 till 17:00. As can be observed, from ten:.