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Delay, Doppler, and amplitude characteristics of HF signals received over a 1300-km transauroral sky wave channel

机译:在1300公里跨极光天波信道上接收到的HF信号的延迟,多普勒和幅度特性

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Channel probe observations of propagation conditions along a 1294-km transauroral path between Sondrestrom, Greenland, and Keflavik, Iceland, were made during the period from March 13 to April 2, 1992. The midpoint of this path was located at a corrected geomagnetic latitude of 12°. The objective of these measurements was to supplement the existing data base describing propagation conditions on the HF transauroral channel with data pertaining to a period around the time of solar maximum. Received signals for this path fell into three distinct groups depending on their amplitude and delay and Doppler spread characteristics. These are (1) strong, specularly reflected ionospheric returns characteristic of a quiescent daytime ionospheric channel during magnetically quiet conditions; (2) strong specular multipath signals reflected from horizontal gradients of electron density and regularly encountered at night; and (3) weak scatter returns that are also a persistent nighttime phenomenon. The scatter returns are usually observed at delays exceeding those anticipated for the one-hop return and, very often, at frequencies that are well above the MUF for the great circle propagation path. The multipath and scatter returns exhibit large delay and Doppler spreads indicative of spatially extensive distributions of drifting and randomly moving irregularities. Two measurement events are discussed which illustrate these conclusions: a noontime measurement with Kp = 3, and a midnight measurement with Kp = 2. The noontime measurement exhibited a scatter return from an isolated irregularity region in addition to the usual ionospheric reflected signals. A simple irregularity drift model produced delay and Doppler shift curves that were consistent with those observed for the scatter component of the received signal and supported a hypothesis of an irregularity region drift speed of 1200 m s parallel to the great circle propagation path.
机译:在1992年3月13日至4月2日期间,对格陵兰岛桑德斯特罗斯特罗姆和冰岛凯夫拉维克之间1294公里跨极光路径的传播条件进行了通道探针观测。该路径的中点位于校正后的地磁纬度12°。这些测量的目的是用与太阳最大时间前后某个时期有关的数据来补充描述HF跨极光信道传播条件的现有数据库。该路径的接收信号根据其幅度和延迟以及多普勒扩展特性分为三个不同的组。这些是(1)在磁性静噪条件下,静态白天电离层通道具有强烈的镜面反射电离层返回特性; (2)从电子密度的水平梯度反射并在夜间经常遇到的强镜面多径信号; (3)分散的回报薄弱,这也是持续存在的夜间现象。通常在超过一跳返回预期的延迟的情况下观察到散射返回,并且通常在远大于大圆传播路径的MUF的频率下观察到散射返回。多径和散射回波表现出较大的延迟,并且多普勒扩展表示漂移和随机运动的不规则性在空间上的广泛分布。讨论了两个测量事件,这些事件说明了这些结论:Kp = 3的午间测量和Kp = 2的午夜测量。除通常的电离层反射信号外,中午测量还显示出从孤立的不规则区域散射回来。一个简单的不规则漂移模型产生的延迟和多普勒频移曲线与所接收信号的散射分量所观察到的一致,并支持一个假设,即平行于大圆传播路径的不规则区域漂移速度为1200 m s。

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