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A model for the multipath delay profile of fixed wireless channels

机译:固定无线信道的多径延迟分布模型

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This paper deals with the measurement and modeling of multipathndelay on fixed wireless paths at 1.9 GHz in suburban environments. Thenprimary focus is on the delay profile, which is the normalized plot ofnreceived power versus delay in response to an RT “impulse.”nWe describe measurement campaigns in the western suburbs of Chicago, IL,nand in suburban north-central New Jersey. Our analysis of the datansuggests to us that, for directive terminal antennas, the delay profilencan be modeled as having a “spike-plus-exponential” shape,ni.e., a strong return (“spike”) at the lowest delay, plus anset of returns whose mean powers decay exponentially with delay. Thisndelay profile can be characterized by just two parameters (both variablenover the terrain), namely, the ratio (K0) of the averagenpowers in the “spike” and “exponential”ncomponents and the decay time constant (Τ0) of then“exponential” component. No such simple structure appears tonapply for delay profiles using omnidirectional antennas. For a directivenantenna with a 32° beamwidth, we find that: (1) the statisticalncorrelation between the profile parameters K0 and Τ0n is negligible; (2) these parameters are relatively insensitive tonantenna height and path length; and (3) over each measured regionn(Illinois and New Jersey), K0 and Τ0 havenmedian values close to 8 dB and just below 0.2 Μs, respectively.nMoreover, we have found simple probability distributions that accuratelynportray the variability of K0 and Τ0 over thenterrain
机译:本文针对郊区环境中1.9 GHz固定无线路径上的多路径延迟进行测量和建模。然后主要关注延迟曲线,这是响应RT“脉冲”的未接收功率与延迟的标准化曲线。n我们描述了伊利诺伊州芝加哥西郊区和新泽西州中北部郊区的测量活动。我们对数据的分析表明,对于定向终端天线,可以将延迟曲线建模为具有“尖峰加指数”形状,即在最小延迟时具有很强的收益(“尖峰”),再加上一组收益,其平均功效随延迟呈指数下降。该延迟分布可以仅通过两个参数(在整个地形上都是可变的)来表征,即“尖峰”和“指数” n分量的平均n功率之比(K0)和当时“指数”分量的衰减时间常数(Τ0) 。对于使用全向天线的延迟分布,没有这种简单的结构适用于延迟分布。对于具有32°波束宽度的定向天线,我们发现:(1)轮廓参数K0和Τ0n之间的统计n相关可忽​​略不计; (2)这些参数是相对不敏感的音高和路径长度; (3)在每个被测区域(伊利诺伊州和新泽西州),K0和Τ0的中值分别接近8 dB,略低于0.2μs。此外,我们发现了简单的概率分布,准确地描述了K0和Τ0在地形上的变化

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