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Frequency dependence of slant path rain attenuations at 15 and 35 GHz

机译:斜路径降雨衰减在15和35 GHz时的频率依赖性

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The main objective of this paper is to examine the frequency dependence of slant path rain attenuation at 15 and 35 GHz in order to determine how well the attenuation at one frequency can be predicted from that at another; this has application in the design of earth-to-satellite communications. Also, some inferences on the drop size distribution of rain can be drawn from simultaneous attenuation measurements at two frequencies. The theory of rain attenuation is reviewed, and it is noted that the attenuation is a complex function of drop size, shape, orientation, index of refraction, and rain intensity along the path. Attenuation ratios are computed on the basis of both drop size and rain rate for frequencies at which there are measured data. Results obtained by other investigators are reviewed, and it is found that frequently, attenuation ratios that would not have been predicted on the basis of a surface rain model such as a Laws and Parsons model have been reported; indications are that attenuation is often produced from a widely dispersed distribution of large raindrops. During eight rainy days in 1975–1976, more than 10,000 simultaneous measurements of 15- and 35-GHz attenuations were recorded in the Boston area. On the basis of these results it is concluded that it is not possible to represent the drop size distribution of rain along a slant path in the Boston area by a Laws and Parsons model, since the ratios of the 35-GHz attenuations to the 15-GHz attenuations are significantly below those that would have been predicted by that model. The ability to predict slant path rain attenuation at one frequency on the basis of that at another is shown to be a function of frequency separation, climatology, and the type of statistics which are desired.
机译:本文的主要目的是研究15和35 GHz斜路径降雨衰减的频率依赖性,以确定可以从一个频率对另一个频率进行预测的程度。这已应用于地球到卫星通信的设计中。同样,可以从两个频率的同时衰减测量得出关于雨滴大小分布的一些推论。回顾了降雨衰减的理论,并注意到,该衰减是沿着路径的液滴大小,形状,方向,折射率和降雨强度的复杂函数。衰减比是根据液滴大小和降雨率计算得出的,这些频率是测量数据的频率。对其他研究者的研究结果进行了回顾,发现经常有报道说,根据劳斯和帕森斯模型等地表降雨模型无法预测衰减率。有迹象表明,衰减通常是由于大雨滴的广泛分布而产生的。在1975年至1976年的八个雨天中,波士顿地区记录了10,000次同时测量的15 GHz和35 GHz衰减。根据这些结果,可以得出结论:由于35 GHz衰减与15 GHz衰减之比,不可能用Laws and Parsons模型来表示波士顿地区沿倾斜路径的雨滴大小分布。 GHz衰减明显低于该模型所预测的衰减。在一个频率的基础上预测一个频率的斜径降雨衰减的能力显示为频率分离,气候学和所需统计类型的函数。

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