Kinetic power components; additionally, its maximum values have been observed following midnight (01:002:00), and inside the morning (09:002.00) and evening hours (18.002:00). That is explained by the influence from the underlying surface. At altitudes of 2500 m, the ratio of the turbulent for the mean kinetic wind power weakly depended around the altitude, except the period after midnight (00:002:00). The character from the altitude dependence changed at evening (03:004:00), in the afternoon (14:005:00), and late within the evening (21:002:00). At altitudes below 100 m, the contribution with the turbulent kinetic wind energy element was small, plus the ratio (z) was in the variety 0.010. The diurnal behavior in the Umov vector depended both on the time in the day and also the sounding altitude. 3 layers have been clearly distinguished: the near-surface layer at altitudes of 55 m, the intermediate layer at altitudes from 15 m to 150 m, and the layer of enhanced turbulence above. The irregular behavior from the kinetic energy flux vector within the near-surface layer was explained by the impact of your underlying surface. Within the intermediate layer whose altitude very first increased from 25 m at 01:00 to 100 m at 03:00, the power transfer inside the north-western path prevailed. From 05:00 until 15:00, the direction of energy transfer changed to south-western with simultaneous increase of the altitude of your intermediate layer to 150 m. Then, from 15:00 till 18:00, the direction of energy transfer remained unchanged, however the decrease boundary from the layer of enhanced turbulence decreased to 100 m. From 19:00 until 22:00, the path of energy transfer changed to north-western, plus the reduced boundary on the layer of enhanced turbulence decreased to 75 m. From 23:00 until 24:00, the power within the lower layer was transferred in the east-southern direction. Above this layer, within the layer of enhanced turbulence, the character of energy transfer changed radically, the kinetic energy flux density enhanced sharply, plus the direction of power transfer fluctuated N-(3-Azidopropyl)biotinamide Protocol resulting from a greater contribution with the turbulent kinetic energy element. The maximum kinetic energy flux densities had been observed at 18:00, when the kinetic energy was predominantly transferred in the south-western path. The spatiotemporal dynamics in the Umov vector may be applied to elucidate time periods and altitude ranges of its N-Methylnicotinamide Endogenous Metabolite maximal and minimal values also as prevailing directions of total kinetic power transfer, that is definitely, to detect occasions and altitudes most and least favorable for flights of unmanned aerial cars, to estimate the effect of wind on high-rise buildings, and to predict the wind energy possible of wind turbines.Author Contributions: Conceptualization, A.P., N.K. and L.S.; methodology, A.P., N.K. and L.S.; computer software, A.P., N.K. and L.S.; validation, A.P., N.K. and L.S.; formal evaluation, A.P., N.K. and L.S.; investigation, A.P., N.K. and L.S.; resources, A.P., N.K. and L.S.; information curation, A.P., N.K. and L.S.; writing–original draft preparation, A.P., N.K. and L.S.; writing–review and editing, A.P., N.K. and L.S.; visualization, A.P., N.K. and L.S.; supervision, A.P., N.K. and L.S.; project administration, A.P., N.K. and L.S.; funding acquisition, A.P., N.K. and L.S. All authors have read and agreed for the published version in the manuscript. Funding: This analysis was carried out together with the financial help in the Russian Academy of Sciences within the framework in the State Assignment towards the Institute of.