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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Relativistic Electron Precipitation Driven by Nonlinear Resonance With Whistler-Mode Waves
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Relativistic Electron Precipitation Driven by Nonlinear Resonance With Whistler-Mode Waves

机译:相对论电子降水受与Whistler-Mode波非线性共振

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Electron losses from the outer radiation belt are typically attributed to resonant electron scattering by whistler-mode waves. Although the quasi-linear diffusive regime of such scattering is well understood, the observed waves are often quite intense and in the nonlinear regime of resonant wave-particle interaction. Such nonlinear resonant interactions are still being actively studied due to their potential for driving fast precipitation. However, direct observations of nonlinear resonance of whistler-mode waves with electron distributions are scarce. Here, we present evidence for such resonance with high-resolution electron energy and pitch angle spectra acquired at low-altitudes by the dual Electron Losses and Fields INvestgation (ELFIN) CubeSats combined with conjugate measurements of equatorial plasma parameters, wave properties, and electron energy spectra by the Time History of Events and Macroscale Interactions during Substorms and Magnetospheric MultiScale missions. ELFIN has obtained numerous conjunction events exhibiting whistler wave driven precipitation; in this study, we present two such events which epitomize signatures of nonlinear resonant scattering. A test particle simulation of electron interactions with intense whistler-mode waves prescribed at the equator is employed to directly compare modeled precipitation spectra with ELFIN observations. We show that the observed precipitating spectra match expectations to within observational uncertainties of wave amplitude for reasonable assumptions of wave power distribution along the magnetic field line. These results indicate the importance of nonlinear resonant effects when describing intense precipitation patterns of energetic electrons and open the possibility of remotely investigating equatorial wave properties using just properties of precipitation energy and pitch angle spectra.
机译:电子损失外辐射带通常归因于共振电子由whistler-mode散射波。准线性扩散政权的散射很好理解,经常观察到的波吗很强烈的非线性机制共振波粒相互作用。非线性共振相互作用仍在积极研究由于他们的潜力开快车降水。观测的非线性共振whistler-mode波和电子分布是稀缺的。与高分辨率电子能量共振在低空和螺距角谱获得的由双电子损失和字段基础(矮)立方体卫星结合赤道的共轭测量等离子体参数、波动性和电子能量时间的历史事件和光谱在亚暴和宏观尺度相互作用磁性层的多尺度任务。结合事件表现出的结果惠斯勒波驱动的降水;研究中,我们提出两个概括这类事件签名的非线性共振散射。测试粒子模拟电子的相互作用以强烈的whistler-mode波规定赤道是用来直接比较建模与矮降水谱观察。沉淀光谱匹配预期内波的观测不确定性振幅波的合理的假设沿着磁场线配电。这些结果表明的重要性在描述非线性共振效应强烈的精力充沛的降水模式远程电子和开放的可能性调查赤道波属性使用只是降水能源和沥青的性质角谱。

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