WIND FACTOR IN SPATIAL AND TEMPORAL DYNAMICS OF WIND EROSION WITHIN VOLYN REGION

B. Matviychuk, N. Matviychuk
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Abstract

The analysis of the wind factor as a factor of wind erosion of Polissia soils is highlighted. The highest intensity of wind erosion in the Polissya zone is observed in the spring and autumn periods, when the density of vegetation cover is the lowest during the year and there is no snow cover. The temporal dynamics of the wind regime forms certain patterns, which determines the formation of the corresponding clusters of months of the year as indicators of the temporal regularity of the wind regime and clusters of administrative districts as indicators of the spatial regularity of the wind regime. The early spring period is the least long (two months), which allows it to be interpreted as transitional. This interpretation explains the inclusion in this cluster by the dynamic features of August as also the transition period from the summer wind regime to the autumn one. The winter period is characterized by an extremely strong wind regime, the lowest wind intensity is observed in the summer-autumn period. The transitional early spring period is characterized by an intermediate level of wind load, but the greatest variability of indicators, which also emphasizes the transitional nature of this time stage of the year. It was established that the maximum value of the wind factor for these areas is observed in winter and is  3,57  m3  s−3,  and  the minimum  is observed in  August and is 2,3 3,57 m3 s−3. The central and eastern regions (Manevytskyi, Kovelskyi and Rozhishchenskyi) also form a homogeneous subzone, the peculiarity of which is that the duration of strong winds in the winter period is somewhat shorter compared to the northwestern regions. The highest wind load is observed in the winter months, and the lowest at the end of summer. Geographically, the north-western and south-eastern regions of the region experience the greatest wind load. In terms of time, three consecutive periods can be distinguished: winter, early spring, and summer-autumn.
volyn地区风蚀时空动态的风因子
重点分析了风因子对波兰土壤风蚀的影响。波利西亚区风蚀强度最大的季节是春季和秋季,这两个季节植被覆盖密度最低,没有积雪覆盖。风势的时间动态形成了一定的模式,这就决定了相应的月份集群的形成,作为风势的时间规律性指标和行政区划集群作为风势的空间规律性指标。早春时期是最短的(两个月),这使得它可以被解释为过渡时期。这一解释解释了8月份的动态特征,也解释了从夏季风向到秋季风向的过渡时期。冬季风势特别强,夏秋两季风强度最低。过渡性早春期的风荷载处于中等水平,但各项指标的变异性最大,这也强调了早春期的过渡性。结果表明,这些地区的风因子在冬季最大值为3.57 m3 s−3,在8月份最小值为2.3357 m3 s−3。中东部地区(Manevytskyi, Kovelskyi和Rozhishchenskyi)也形成了一个均匀的分区,其特点是冬季强风的持续时间比西北地区短一些。冬季风荷载最大,夏末风荷载最小。从地理上看,该地区的西北和东南地区风负荷最大。在时间上,可以区分出三个连续的时期:冬季、早春和夏秋。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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