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Interpretation of angle-of-arrival measurements in the lower atmosphere using spaced antenna radar systems

机译:使用间隔天线雷达系统解释低层大气中的到达角测量

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On the basis of scattering theory, we present four different contributions to angle-of-arrival (AOA) measurements using spaced antenna (SA) radar systems. We show that the measurement of the scattering parameters is needed to estimate most AOA contributions (e.g., tilt angle of layers). We analyze a general SA system (i.e., receiving antennas not necessarily symmetrically placed about the transmitter) and show, theoretically, that such systems can be used for vertical velocity corrections without explicitly knowing the scattering parameters (e.g., correlation lengths). The theoretical AOA expressions are compared with lower atmospheric data (3-21 km) obtained with the Jicamarca VHF radar system in Perú. We compare the AOAs obtained by a time and a frequency domain method, giving both methods essentially the same information. While the results are comparable, frequency domain AOAs tend to exhibit more “outliers.” Prom examination of time series of these AOA measurements, we find some short, but predominantly long-period oscillations (>12 hours) with amplitudes of ∼1°.
机译:基于散射理论,我们对使用间隔天线(SA)雷达系统的到达角(AOA)测量提出了四种不同的贡献。我们表明需要测量散射参数来估计大多数AOA贡献(例如,层的倾斜角)。我们分析了一般的SA系统(即接收天线不一定对称地放置在发射机周围),并从理论上证明了此类系统可用于垂直速度校正,而无需明确知道散射参数(例如相关长度)。将理论的AOA表达式与秘鲁的Jicamarca VHF雷达系统获得的较低大气数据(3-21 km)进行了比较。我们比较了通过时域和频域方法获得的AOA,为这两种方法提供了基本相同的信息。尽管结果是可比的,但频域AOA往往表现出更多的“离群值”。对这些AOA测量的时间序列进行舞会检查,我们发现一些短暂但主要是长周期的振荡(> 12小时),振幅约为1°。

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