3-Methylbenzaldehyde Biological Activity kinetic energy elements; furthermore, its maximum values were observed 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 from the turbulent for the imply kinetic wind power weakly depended on the altitude, except the period after midnight (00:002:00). The character in the 3-Hydroxybenzaldehyde manufacturer altitude dependence changed at evening (03:004:00), inside the afternoon (14:005:00), and late in the evening (21:002:00). At altitudes below 100 m, the contribution on the turbulent kinetic wind power component was smaller, and the ratio (z) was inside the variety 0.010. The diurnal behavior in the Umov vector depended each around the time on the day along with 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 also 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 on the underlying surface. Within the intermediate layer whose altitude very first enhanced from 25 m at 01:00 to 100 m at 03:00, the energy transfer inside the north-western direction prevailed. From 05:00 until 15:00, the path of energy transfer changed to south-western with simultaneous boost with the altitude of your intermediate layer to 150 m. Then, from 15:00 until 18:00, the path of energy transfer remained unchanged, but the reduced boundary of the layer of enhanced turbulence decreased to 100 m. From 19:00 till 22:00, the direction of power transfer changed to north-western, and also the reduce boundary of your layer of enhanced turbulence decreased to 75 m. From 23:00 until 24:00, the power within the decrease 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 enhanced sharply, and the direction of power transfer fluctuated due to a higher contribution of the turbulent kinetic power component. The maximum kinetic power flux densities were observed at 18:00, when the kinetic power was predominantly transferred in the south-western direction. The spatiotemporal dynamics from the Umov vector can be applied to elucidate time periods and altitude ranges of its maximal and minimal values at the same time as prevailing directions of total kinetic power transfer, that may be, to detect instances and altitudes most and least favorable for flights of unmanned aerial automobiles, to estimate the impact of wind on high-rise buildings, and to predict the wind power potential of wind turbines.Author Contributions: Conceptualization, A.P., N.K. and L.S.; methodology, A.P., N.K. and L.S.; software program, 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.; 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 study and agreed for the published version from the manuscript. Funding: This analysis was carried out using the financial help with the Russian Academy of Sciences within the framework with the State Assignment for the Institute of.
