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RADIO SOUNDING SCIENCE AT HIGH POWERS

机译:高功率无线电测深科学

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摘要

Future space missions like the Jupiter Icy Moons Orbiter (JIMO) planned to orbit Callisto, Ganymede, and Europa can fully utilize a variable power radio sounder instrument. Radio sounding at 1 kHz to 10 MHz at medium power levels (10 W to kW) will provide long-range magnetospheric sounding (several Jovian radii) like those first pioneered by the radio plasma imager instrument on IMAGE at low power (<10 W) and much shorter distances (<5 R_E). A radio sounder orbiting a Jovian icy moon would be able to globally measure time-variable electron densities in the moon ionosphere and the local magnetospheric environment. Near-spacecraft resonance and guided echoes respectively allow measurements of local field magnitude and local field line geometry, perturbed both by direct magnetospheric interactions and by induced components from subsurface oceans. JIMO would allow radio sounding transmissions at much higher powers (~10 kW) making subsurface sounding of the Jovian icy moons possible at frequencies above the ionosphere peak plasma frequency. Subsurface variations in dielectric properties, can be probed for detection of dense and solid-liquid phase boundaries associated with oceans and related structures in overlying ice crusts.
机译:计划向卡里斯托,木卫三和欧罗巴轨道运行的木星冰月卫星(JIMO)等未来的太空任务可以充分利用可变功率无线电测深仪。在中等功率水平(10 W到kW)下以1 kHz到10 MHz进行无线电探测将提供远距离的磁层探测(几个Jovian半径),就像无线电等离子体成像仪首次在低功率(<10 W)的IMAGE上首次提出的那样。和更短的距离(<5 R_E)。绕着Jovian冰冷月球运行的无线电探空仪将能够整体测量月球电离层和局部磁层环境中随时间变化的电子密度。近太空飞船的共振和引导的回波分别允许测量局部场的大小和局部场线的几何形状,它们会受到直接的磁层相互作用和地下海洋感应成分的干扰。 JIMO将允许以更高的功率(〜10 kW)进行无线电探测,从而在电离层峰值等离子体频率以上的频率下实现木星冰月卫星的地下探测。可以探测地下介电特性的变化,以检测与上覆冰壳中的海洋和相关结构相关的致密和固液相边界。

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