Kinetic energy components; in addition, its Ecabet (sodium) Purity & Documentation maximum values have been observed right after midnight (01:002:00), and inside the morning (09:002.00) and evening hours (18.002:00). This is explained by the influence of your underlying surface. At altitudes of 2500 m, the ratio from the turbulent for the mean kinetic wind energy weakly depended on the altitude, except the period right after midnight (00:002:00). The character in the Petunidin (chloride) web altitude dependence changed at evening (03:004:00), inside the afternoon (14:005:00), and late in the evening (21:002:00). At altitudes beneath 100 m, the contribution on the turbulent kinetic wind energy element was tiny, as well as the ratio (z) was in the range 0.010. The diurnal behavior on the Umov vector depended each around the time from the day and the sounding altitude. Three layers were 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 of your kinetic energy flux vector in the near-surface layer was explained by the effect of your underlying surface. Inside the intermediate layer whose altitude initial increased from 25 m at 01:00 to 100 m at 03:00, the power transfer within the north-western direction prevailed. From 05:00 till 15:00, the path of energy transfer changed to south-western with simultaneous raise in the altitude from the intermediate layer to 150 m. Then, from 15:00 until 18:00, the direction of energy transfer remained unchanged, but the lower boundary of your layer of enhanced turbulence decreased to one hundred m. From 19:00 until 22:00, the path of power transfer changed to north-western, and also the decrease boundary in the layer of enhanced turbulence decreased to 75 m. From 23:00 till 24:00, the energy 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 power flux density elevated sharply, along with the path of power transfer fluctuated as a consequence of a greater contribution from the turbulent kinetic power element. The maximum kinetic power flux densities were observed at 18:00, when the kinetic power was predominantly transferred within the south-western path. The spatiotemporal dynamics in the Umov vector might be made use of to elucidate time periods and altitude ranges of its maximal and minimal values as well as prevailing directions of total kinetic power transfer, which is, to detect occasions and altitudes most and least favorable for flights of unmanned aerial automobiles, to estimate the effect of wind on high-rise buildings, and to predict the wind energy potential of wind turbines.Author Contributions: Conceptualization, A.P., N.K. and L.S.; methodology, A.P., N.K. and L.S.; software, A.P., N.K. and L.S.; validation, A.P., N.K. and L.S.; formal analysis, A.P., N.K. and L.S.; investigation, A.P., N.K. and L.S.; sources, 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 acquisition, A.P., N.K. and L.S. All authors have read and agreed to the published version in the manuscript. Funding: This study was carried out using the economic support of your Russian Academy of Sciences inside the framework on the State Assignment to the Institute of.
