Kinetic power elements; in addition, its maximum values had been observed just after midnight (01:002:00), and within the morning (09:002.00) and evening hours (18.002:00). This really is explained by the influence of your underlying surface. At altitudes of 2500 m, the ratio on the turbulent for the imply kinetic wind power weakly depended on the altitude, except the period immediately after midnight (00:002:00). The character of your altitude dependence changed at evening (03:004:00), in the afternoon (14:005:00), and late in the evening (21:002:00). At altitudes beneath one hundred m, the contribution in the turbulent kinetic wind energy component was tiny, along with the ratio (z) was in the range 0.010. The diurnal behavior from the Umov vector depended both around the time with the day and also the sounding altitude. Three 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 also the layer of enhanced turbulence above. The irregular behavior in the kinetic power flux vector within the near-surface layer was explained by the effect from the underlying surface. In the intermediate layer whose altitude first elevated from 25 m at 01:00 to one hundred m at 03:00, the power transfer Nipecotic acid Purity inside the north-western path prevailed. From 05:00 till 15:00, the path of energy transfer changed to south-western with simultaneous increase from the altitude of the intermediate layer to 150 m. Then, from 15:00 till 18:00, the path of power transfer remained unchanged, but the lower boundary of the layer of enhanced turbulence decreased to one hundred m. From 19:00 until 22:00, the direction of energy transfer changed to north-western, and also the lower boundary from the layer of enhanced turbulence decreased to 75 m. From 23:00 till 24:00, the power in the reduce layer was transferred inside the east-southern direction. Above this layer, within the layer of enhanced turbulence, the character of energy transfer changed radically, the kinetic power flux density increased sharply, as well as the direction of energy transfer fluctuated due to a greater contribution of the turbulent kinetic power component. The maximum kinetic energy flux densities had been observed at 18:00, when the kinetic power was predominantly transferred inside the south-western direction. The spatiotemporal dynamics in the Umov vector might be utilised to elucidate time periods and altitude ranges of its maximal and minimal values too as prevailing directions of total kinetic energy transfer, that is, to detect occasions and altitudes most and least favorable for flights of unmanned aerial autos, to estimate the effect of wind on high-rise buildings, and to predict the wind energy prospective of wind turbines.Author Contributions: Conceptualization, A.P., N.K. and L.S.; methodology, A.P., N.K. and L.S.; application, 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.; data 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 Stearic acid-d3 Formula acquisition, A.P., N.K. and L.S. All authors have read and agreed to the published version from the manuscript. Funding: This research was carried out with the financial assistance of the Russian Academy of Sciences within the framework in the State Assignment to the Institute of.