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Calculation of vertical profile of wind velocity and power of wind flow on desert plains

机译:沙漠平原风速和风功率垂直剖面的计算

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For the atmospheric layer that is swept by the rotors of the wind-driven power plant (WDPP) of medium and high power, we have chosen a numerical technique for calculating the vertical profile of the wind velocity, its statistical characteristics, and also the specific power of the wind flow on the desert plains, the roughness of the underlying surface of which can be assumed to be uniform. The calculation was carried out on the base of decennial wind velocity monitoring at a height of 10 m (the height of the weather vane location) at the Tamdy (Uzbekistan) weather station with account for the variation of the temperature stratification in the course of the day and year. The comparison of the obtained results with the data of the aerologic observations at the weather station and with the main regularities of the variations of the velocity and specific power of the wind flow con- firmed the correctness of the use of the calculation procedure for the specific orographic conditions. [PUBLICATION ABSTRACT]
机译:对于中功率和高功率风力发电厂(WDPP)的转子扫过的大气层,我们选择了一种数值技术来计算风速的垂直剖面,其统计特征以及特定的风在沙漠平原上的力量,可以认为其下表面的粗糙度是均匀的。该计算是根据塔米(乌兹别克斯坦)气象站10 m高度(风向标位置的高度)的十年期风速监测进行的,并考虑了在此过程中温度分层的变化。日和年。将获得的结果与气象站的气象观测数据以及风速和风的比功率变化的主要规律进行比较,从而确定了针对特定目标使用计算程序的正确性地形条件。 [出版物摘要]

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