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Magnetospheric amplification and emission triggering by ELF/VLF waves injected by the 3.6 MW HAARP ionospheric heater

机译:3.6兆瓦HAARP电离层加热器注入的ELF / VLF波触发了磁层的放大和发射

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The HF dipole array of the High Frequency Active Auroral Research Program (HAARP) in Gakona, Alaska, was recently upgraded to 180 elements, facilitating operations at a total radiated power level of 3.6 MW and an effective radiated power of ~575 MW. In the first experiments at the new power level, the HAARP array is used for magnetospheric wave injection. Modulated heating of auroral electrojet currents in the ionosphere yields radiation in the ELF/VLF frequency range. The HAARP-generated signals are injected into the magnetosphere, where they propagate in the whistler mode in field-aligned “ducts,” allowing them to be observed at the conjugate point on a ship-borne receiver and on autonomous buoy platforms. The observation of the 1-hop signals is accompanied by the observation of associated 2-hop components in the northern hemisphere, which have reflected from the ionospheric boundary in the southern hemisphere. The observed signals are accompanied by triggered emissions and exhibit temporal amplification of 15–25 dB/s and bandwidth broadening to ~50 Hz. Amplification occurs at injected signal frequencies selected in near real time on the basis of observations of natural emission activity, and only certain components of the frequency-time formats transmitted are amplified. Observations at multiple sites and dispersion analysis show that the signals are injected into the magnetosphere directly above the HF heater. The duration of echo observation and the prevalence of 1-hop observations are consistent with statistics from 1986 Siple Station experiments. The particle-trapping wave amplitude near the magnetic equator is estimated in the range 0.1–0.4 pT and gyroresonance with 10 keV–100 keV electrons.
机译:最近,阿拉斯加加科纳市的高频有源极光研究计划(HAARP)的高频偶极子阵列已升级为180个元件,以总辐射功率为3.6兆瓦,有效辐射功率为575兆瓦的功率运行。在新功率级别的第一个实验中,HAARP阵列用于磁层波注入。电离层中的极光电喷射电流的调制加热产生ELF / VLF频率范围内的辐射。 HAARP产生的信号被注入磁层,在此以惠斯勒模式在场对准的“管道”中传播,从而可以在船载接收器和自主浮标平台上的共轭点处观察到它们。对1跳信号的观察与对北半球相关2跳分量的观察伴随,这些分量已从南半球的电离层边界反射。观测到的信号伴随着触发发射,并表现出15–25 dB / s的时间放大,带宽扩展到〜50 Hz。放大会在观察自然发射活动的基础上以几乎实时选择的注入信号频率发生,并且仅放大传输的频率-时间格式的某些分量。在多个位置的观察和色散分析表明,信号被注入到HF加热器正上方的磁层中。回波观测的持续时间和1跳观测的普遍性与1986年Siple站实验的统计数据一致。磁赤道附近的粒子俘获波幅度估计在0.1–0.4 pT范围内,并具有10 keV–100 keV电子的回旋共振。

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