Urface layer at altitudes of 55 m, an intermediate layer at altitudes from 15 m to 150 m, and From 23:00 until 24:00, the power within the decrease layer was transferred in the eastsouth a layer of enhanced turbulence above. The irregular behavior in the kinetic energy flux ern direction. Above this layer, in the layer of enhanced turbulence, the character of en vector within the near-surface layer is explained by the effect with the underlying surface. In ergy transfer changed Ecabet (sodium) Description radically, the kinetic energy flux density improved sharply, along with the the intermediate layer whose altitude zturb 1st enhanced from 25 m at 01:00 to 100 m at direction of power transfer fluctuated resulting from a higher contribution from the turbulent ki 03:00, the power transfer within the north-western path prevailed. From 05:00 till 15:00, the energy of power transfer changed to south-western flux simultaneous raise netic directioncomponent. The maximum kinetic energy with densities have been observed at of zturb to 150 m. Then, from 15:00 till 18:00, the direction of energy transfer remained 18:00, when the kinetic energy was predominantly transferred within the southwestern direc unchanged, but the lower boundary of the layer of enhanced turbulence zturb decreased to tion. From Petunidin (chloride) Autophagy Figure 3 it might be seen that the altitude range z zturb and also the time period from 100 m. From 19:00 until 22:00, the direction of power transfer changed to north-western, 06:00 till 18:00 are most harmful for UAV flights [2]. The wind impact on highrise create and zturb decreased to 75 m. ings becomes most pronounced from 08:00 till 18:00, when the maximum values on the From 23:00 until 24:00, the power within the reduce layer was transferred within the eastsouthern path. Above this layer, within the layer of enhanced turbulence, the character of energy transfer changed radically, the kinetic energy flux density enhanced sharply, as well as the path of energy transfer fluctuated as a result of a greater contribution in the turbulent kinetic energy component. The maximum kinetic power flux densities had been observed at 18:00, when the kinetic energy was predominantly transferred in the south-western path. From Figure three it can be noticed that the altitude variety z zturb and the time period from 06:00 till 18:00 are most risky for UAV flights [2]. The wind effect on high-rise buildings becomes most pronounced from 08:00 till 18:00, when the maximum values from the Umov vector had been observed for z zturb [3]. Meanwhile, these higher values of your Umov vectors are promising for the wind energy possible of wind turbines directly proportional for the average kinetic energy flux density [4,five,17,18].Atmosphere 2021, 12,10 of5. Conclusions Based on post-processing of your information of minisodar measurement, a novel system of investigating the spatiotemporal dynamics with the kinetic power flux density vector–the Umov vector–has been proposed and effectively realized. The diurnal hourly behavior on the vertical profiles in the imply and turbulent kinetic energy components and also the wind velocity vector field within the reduced 200-m layer with the atmosphere had been analyzed together using the ratio from the turbulent to imply kinetic power elements. At night and morning hours (00:004:00), (z) was within the variety 0.0100; inside the evening, the span of its values increased to 0.01000, after which due to the fact 23:00, it decreased once more to 0.0100. In the nearground layer, at altitudes as much as 25 m, attention is drawn to sharp changes with the ratio in the.
