Urface layer at altitudes of 55 m, an intermediate layer at altitudes from 15 m

Urface layer at altitudes of 55 m, an intermediate layer at altitudes from 15 m to 150 m, and From 23:00 till 24:00, the power in the lower layer was transferred 1-Dodecanol Purity & Documentation within the eastsouth a layer of enhanced turbulence above. The irregular behavior of your kinetic power flux ern direction. Above this layer, in the layer of enhanced turbulence, the character of en vector in the near-surface layer is explained by the impact of the underlying surface. In ergy transfer changed radically, the kinetic energy flux density enhanced sharply, and the the intermediate layer whose altitude zturb first enhanced from 25 m at 01:00 to 100 m at path of power transfer fluctuated on account of a higher contribution in the turbulent ki 03:00, the energy transfer within the north-western direction prevailed. From 05:00 till 15:00, the energy of energy transfer changed to south-western flux simultaneous boost netic directioncomponent. The maximum kinetic power with densities have been observed at of zturb to 150 m. Then, from 15:00 till 18:00, the path of power transfer remained 18:00, when the kinetic energy was predominantly transferred in the southwestern direc unchanged, however the reduce boundary on the layer of enhanced turbulence zturb decreased to tion. From Figure three it could be noticed that the altitude variety z zturb and the time period from 100 m. From 19:00 till 22:00, the direction of energy transfer changed to north-western, 06:00 till 18:00 are most unsafe for UAV flights [2]. The wind effect on highrise build 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 inside the eastsouthern direction. Above this layer, within the layer of enhanced turbulence, the character of power transfer changed radically, the kinetic power flux density enhanced sharply, and also the path of energy transfer fluctuated due to a higher contribution of the turbulent kinetic energy element. The maximum kinetic energy flux densities have been observed at 18:00, when the kinetic energy was predominantly transferred within the south-western direction. From Figure 3 it can be observed that the altitude range z zturb and also the time period from 06:00 till 18:00 are most harmful for UAV flights [2]. The wind effect on high-rise buildings becomes most pronounced from 08:00 till 18:00, when the maximum values with the Umov vector have been observed for z zturb [3]. Meanwhile, these higher values of your Umov vectors are promising for the wind energy possible of wind turbines straight proportional for the average kinetic power flux density [4,five,17,18].Atmosphere 2021, 12,ten of5. Conclusions Primarily based on post-processing of your information of minisodar measurement, a novel technique of investigating the spatiotemporal dynamics on the kinetic energy flux density vector–the Umov vector–has been proposed and successfully realized. The diurnal hourly behavior with the vertical (S)-Amlodipine besylate custom synthesis profiles of your mean and turbulent kinetic power elements and the wind velocity vector field in the reduced 200-m layer of the atmosphere had been analyzed with each other with the ratio from the turbulent to mean kinetic power components. At evening and morning hours (00:004:00), (z) was within the variety 0.0100; in the evening, the span of its values enhanced to 0.01000, then considering the fact that 23:00, it decreased again to 0.0100. Inside the nearground layer, at altitudes up to 25 m, attention is drawn to sharp changes from the ratio from the.