首页> 外文期刊>Geophysical Research Letters >Guided echoes in the magnetosphere: Observations by Radio Plasma Imager on IMAGE - art. no. 1589
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Guided echoes in the magnetosphere: Observations by Radio Plasma Imager on IMAGE - art. no. 1589

机译:磁层中的引导回波:无线电等离子体成像仪对IMAGE的观察-艺术。没有。 1589

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1] Long-range, discrete, radio echo traces observed in the magnetosphere by the Radio Plasma Imager (RPI) on IMAGE have been interpreted as signals guided along geomagnetic field lines. During IMAGE traversals of the plasmapause and near-equatorial plasmasphere, multiple echo traces, attributed to signals reflected successively between conjugate hemispheres, are often observed. Single traces seen far beyond the plasmapause at high latitudes are attributed to guided echoes from the local hemisphere in the polar region. Here the field lines are either (1) open, (2) closed but too long to be observed within the instrument listening time or (3) closed but not able to maintain the signal-guiding conditions across the equator to the conjugate hemisphere. In this letter we present examples of guided echoes producing both the single and multiple reflection traces observed by RPI at altitudes of a few Earth radii and discuss possible guiding mechanisms. [References: 23
机译:1]通过IMAGE上的放射性等离子体成像仪(RPI)在磁层中观察到的远距离,离散的无线电回波轨迹已被解释为沿地磁场线引导的信号。在等离子暂停和近赤道等离子层的IMAGE遍历过程中,经常观察到多条回波痕迹,这些痕迹归因于在共轭半球之间连续反射的信号。在高纬度地区,远距离等离子暂停处看到的单条迹线归因于来自极地局部半球的引导回波。在这里,磁力线要么是(1)打开,(2)是闭合的,但是太长而无法在仪器收听时间内被观察到,或者(3)是闭合的,但不能维持跨赤道到共轭半球的信号引导条件。在这封信中,我们提供了一些示例性的引导回波,这些引导回波产生了RPI在几个地球半径的高度上观察到的单反射和多反射迹线,并讨论了可能的引导机制。 [参考:23

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