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Formation of lower-hybrid solitary structures by modulational interaction between lower-hybrid and dispersive Alfvén waves

机译:通过低杂波与色散Alfvén波之间的调制相互作用形成低杂波孤立结构

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We investigate the possibility that lower-hybrid solitary structures (LHSS), which are frequently observed in the Earth's ionosphere and magnetosphere, are formed as a result of a modulational interaction between lower-hybrid and dispersive Alfvén waves of initially small amplitude. A large amplitude lower-hybrid pump wave can excite density structures with length scales transverse to the geomagnetic field of the order of the ion gyroradius via a modulational instability. The structure formation in the nonlinear stage of the instability is investigated by numerical solutions of the governing equations, using plasma parameters relevant for LHSS observations in the upper ionosphere and in the magnetosphere. The numerical solutions reveal that the lower-hybrid waves become self-localized inside cylindrically symmetric (with respect to the ambient magnetic field) density cavities, in qualitative agreement with observations. Our model includes thermal electron effects but shows no stabilization at the ion sound gyroradius, suggesting that any preference of observed LHSS for that perpendicular scale likely is due to processes arresting the cavity collapse.
机译:我们研究了低杂波孤立结构(LHSS)的可能性,这种杂波在地球电离层和磁层中经常被观察到,这是由于低杂波和分散的Alfvén波之间的调制相互作用而形成的,该调制波最初的振幅很小。大振幅的低杂波泵浦波可以通过调制不稳定性激发长度方向垂直于离子陀螺半径的地磁场的长度尺度的密度结构。使用与上层电离层和磁层中与LHSS观测相关的等离子参数,通过控制方程的数值解研究了非线性不稳定阶段的结构形成。数值解表明,低混合波在圆柱对称(相对于环境磁场)密度腔内变得自定位,与观测结果在质量上一致。我们的模型包括热电子效应,但在离子声回旋半径处没有稳定,这表明观察到的LHSS对于该垂直尺度的任何偏爱很可能是由于阻止空腔塌陷的过程所致。

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