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Rainfall time series synthesis from queue scheduling of rain event fractals over radio links

机译:通过无线电链路上的降雨事件分形的队列调度来合成降雨时间序列

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摘要

Rainfall attenuation over wireless networks stems from random fluctuations in the natural process of arriving rainfall rates over radio links. This arrival process results in discernible rainfall traffic pattern which manifests as naturally scheduled and queue-generated rain spikes. Hence, the phenomenon of rainfall process can be approached as a semi-Markovian queueing process, with event characteristics dependent on queue parameters. However, a constraint to this approach is the knowledge of the physical characteristics of queue-generated rain spikes. Therefore, this paper explores the probability theory and descriptive mathematics of rain spikes in rainfall processes. This investigation presents the synthesis of rainfall queue with rain spikes at subtropical and equatorial locations of Durban (29°52'S, 30°58'E) and Butare (2°36'S, 29°44'E), respectively. The resulting comparative analysis of rainfall distributions, using error analysis at both locations, reveals that queue-generated rainfall compares well with measured rainfall data set. This suggests that the time-varying process of rainfall, though stochastic, can be synthesized via queue scheduling with the application of relevant queue parameters at any location.
机译:无线网络上的降雨衰减源于通过无线电链路到达降雨率的自然过程中的随机波动。此到达过程导致可识别的降雨流量模式,表现为自然调度和队列生成的降雨峰值。因此,降雨过程的现象可以作为半马尔可夫排队过程来处理,事件特征取决于队列参数。但是,这种方法的局限性是要了解队列生成的降雨峰值的物理特性。因此,本文探讨了降雨过程中降雨峰值的概率理论和描述数学。这项研究提出了分别在德班(南纬29°52',东经30°58')和布塔雷峰(南纬2°36',29°44')的亚热带和赤道位置出现的带有降雨峰值的降雨队列。使用两个位置的误差分析对降雨分布进行的比较分析表明,队列生成的降雨与测得的降雨数据集具有很好的比较。这表明降雨的时变过程虽然是随机的,但可以通过在任何位置应用相关队列参数通过队列调度来综合。

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