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Long term azimuth and elevation measurements in the HF band

机译:HF波段的长期方位角和仰角测量

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摘要

Even in the time of satellite communication long distance links in the HF band (3-30 MHz) via the ionosphere are still of great significance. There is also a need for reconnaissance and location in this frequency band. One approach is the single site location (SSL) technique which is capable of estimating the location of transmitters with only one direction finder (DF). A prerequisite for this method is the ability of the DF to measure both azimuth and elevation angle of the incoming wave. This is for example possible by using the interferometric DF. The SSL method works if: the wave is propagating via the ionosphere (sky wave propagation); the virtual height of the ionosphere at the point of reflection is approximately known; and the wave is propagated with a single "hop" (the number of ionospheric reflections) between transmitter and DF. Clearly these assumptions may not be satisfied in practice. If we do not know the position of the transmitter (which is the normal situation in reconnaissance) we will not know the point of reflection. Hence it is not possible to measure or estimate (by means of an appropriate propagation prediction program) the ionospheric behaviour at this point. Furthermore the number of hops is unknown. Nevertheless the SSL method works satisfactory in some cases. We show results from a long term measurement campaign made in the winter of 1995/1996 (azimuth and elevation, signal amplitude) and a measurement campaign in November 1994. The data is used to check the validity of a new prediction program which is actually under development.
机译:即使在进行卫星通信时,通过电离层在HF频段(3-30 MHz)中进行长距离链接仍然具有重要意义。在此频段也需要侦察和定位。一种方法是单站点定位(SSL)技术,该技术能够仅使用一个测向仪(DF)估算发射机的位置。该方法的先决条件是DF能够测量入射波的方位角和仰角。这例如可以通过使用干涉DF来实现。 SSL方法在以下情况下有效:波通过电离层传播(天波传播);反射点电离层的虚拟高度大约是已知的;并且波在发射机和DF之间以单个“跳”(电离层反射的数量)传播。显然,这些假设在实践中可能无法满足。如果我们不知道发射器的位置(这是侦察中的正常情况),我们将不知道反射点。因此,不可能在此时测量或估计(通过适当的传播预测程序)电离层的行为。此外,跳数是未知的。尽管如此,SSL方法在某些情况下仍能令人满意。我们显示了1995/1996年冬季进行的长期测量活动(方位角和仰角,信号幅度)和1994年11月进行的测量活动的结果。这些数据用于检查新的预测程序的有效性,该预测程序实际上在发展。

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