首页> 外文会议>2011 30th URSI General Assembly and Scientific Symposium >Detection of magnetospherically ducted VLF signals geomagnetically conjugate to a Russian Alpha transmitter at L=1.9
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Detection of magnetospherically ducted VLF signals geomagnetically conjugate to a Russian Alpha transmitter at L=1.9

机译:在L = 1.9的情况下,探测磁层导管的VLF信号与俄罗斯Alpha发射机地磁共轭

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The Russian ‘Alpha’ transmitters broadcast alternating pulses between 11–15 kHz for navigation. A fraction of the VLF energy escapes into the magnetosphere, is guided by ducts, amplified by interaction with radiation belt particles, and observed at the geomagnetic conjugate point. We analyze VLF data from Adelaide, Australia, conjugate to Komsomolsk transmitter. An automated detection scheme separates the subionospheric and magnetospheric signals. We track availability of ducts at L=1.9 and find them present often. We correlate to geomagnetic conditions and assess the role of wave growth and triggering from wave-particle interactions, and compare to DEMETER satellite measurements.
机译:俄罗斯的“阿尔法”发射器广播11-15 kHz之间的交替脉冲以进行导航。 VLF能量的一部分逸出进入磁层,由管道引导,与辐射带粒子相互作用而放大,并在地磁共轭点观察到。我们分析了来自澳大利亚阿德莱德的共轭Komsomolsk发射器的VLF数据。自动检测方案将电离层和磁层以下信号分开。我们跟踪L = 1.9处的风管可用性,并发现它们经常出现。我们与地磁条件相关,并评估波的增长和波粒相互作用触发的作用,并与DEMETER卫星测量结果进行比较。

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