广岛和阿索地区因散射e和对流层导管引起的甚高频无线电波异常传播观测

K. Shin, M. Nishi, Teruaki Yoshida
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引用次数: 2

摘要

在非视距甚高频无线电波观测中,经常观测到电离层散射e (Es传播)和对流层导管(对流层导管)引起的异常传播。众所周知,它们会对电视、无线电广播和无线通信造成干扰,因此了解它们是很重要的。为了弄清异常传播的特点,我们在广岛和麻生进行了为期六年的VHF波段超视距调频无线电波观测。对于多年来观测到的大量数据集的分析,对无线电波进行自动分类和提取是很重要的。本文给出了一种对上述两种异常传播进行自动分类的方法。该方法的步骤是基于它们的传播特性和接收到的信号强度。利用双频法分离了异常传播和宽带噪声。为了对该方法进行评价,利用2005 ~ 2010年的观测资料,对该方法探测到的Es传播和对流层导管的发生情况进行了分析。结果表明,Es的繁殖主要发生在夏季,6月和7月是一年中最常见的月份。此外,他们经常在一天的10点到12点和16点到18点被观察到。这些结果与过去在中纬度地区的观测结果具有相同的趋势。另一方面,在春季和秋季,在Aso天文台从晚上到早晨观测对流层管道。这些结果与以往秋季到春季对流层逆温层出现的观测结果一致。相反,在过去观测报告逆温层发生的夏季,对流层导管较少。由于调频无线电波的传播特性已经被清楚地显示出来,证实了该分类方法是有效的。
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Observations of anomalous propagation of VHF radio wave due to sporadic-E and tropospheric duct in Hiroshima and Aso
In non line-of-sight VHF radio wave observation, anomalous propagations due to ionospheric sporadic-E (Es propagation) and tropospheric duct (tropospheric ducting) have been frequently observed. They are known to cause an interference problem in the television, radio broadcasts and wireless communications, so that it is important to understand them. In order to make clear the characteristics of the anomalous propagations, we have observed over-horizon FM radio waves in VHF band for six years in Hiroshima and Aso. For analyses of large amounts of data set observed over years, it is important to classify and extract the radio waves automatically. In this paper, we show a method to classify above two anomalous propagations automatically. Procedures of the method are based on their propagation characteristics and received signal strength. Further the anomalous propagations and broadband noises are separated using dual frequency method. In order to evaluate the method, we examined the occurrence of the Es propagation and tropospheric ducting detected by the above method using the data observed from 2005 to 2010. It was found that the Es propagations were mostly observed in summer season and more frequently observed months in a year were June and July. Further, they were frequently observed from 10 to 12 and from 16 to 18 o’clock in a day. These results had the same tendency as past observations at mid-latitude. On the other hand, the tropospheric ducting was observed from night to morning time in spring and fall at Aso observatory. These results were consistent with past observations of occurrences of inversion layer in the troposphere from fall to spring. In contrast, it was confirmed that there were few tropospheric ducting in summer season while the past observations reported the inversion layer occurred. Since propagation characteristics of the FM radio waves have been clearly shown, it was confirmed that the classification method worked effectively.
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