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Subauroral Flow Channel Structures and Auroral Undulations Triggered by Kelvin-Helmholtz Waves

机译:Subauroral流道结构和极光波动引发的Kelvin-Helmholtz波

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We investigate Kelvin-Helmholtz (K-H) waves on/near the magnetopause and surface waves near the plasmapause-in the outer region of the plasmasphere: in the hot zone-by utilizing multiinstrument/ satellite observations. Our main aim is to study how the K-H waves and the K-H instability mechanisms impacted the subauroral and auroral regions during the geomagnetic storms of May 27-29 and July 16, 2017. For the subauroral region, we specify the structured flows as Sub-Auroral Polarization Streams Wave Structures (SAPS-WS) and the combined flows-created by Abnormal Sub-Auroral Ion Drifts (ASAID) and SAID or SAPS-as a complex equatorward-poleward ASAID-SAID or SAPS-ASAID. For the auroral zone, we identify the large auroral undulations appearing inside the auroral zone. The correlated observations of the K-H waves, the structured or complex subauroral flows and large auroral undulations, and the local geomagnetic field oscillations confirm the connections of both the subauroral flows and the auroral undulations with the K-H waves via the eigenfrequency of the Near-Earth Plasma Sheet (NEPS) resonator activated by the K-H waves. For the first time, we demonstrate the simultaneous detections of K-H waves near the magnetopause and surface waves near the plasmapause in the hot zone on July 16, 2017, and conclude their coupling via the NEPS resonator's eigenfrequency. Thus, the surface waves near the plasmapause were the manifestation of the undulating (or rippled) earthward inner boundary of the NEPS that led to the development of ASAID-SAID/SAPS-ASAID or SAPS-WS in the subauroral region and to the large auroral undulation inside the auroral zone.
机译:我们调查Kelvin-Helmholtz (k - h)附近的磁层和表面波附近plasmapause-in外的区域通过利用等离子体层:热multiinstrument /卫星观测。目的是研究k - h波和k - h不稳定影响了subauroral机制期间和极光地区地磁风暴5月- 7月16日,2017年。subauroral地区,我们指定的结构化流亚极光极化流波结构(SAPS-WS)和总和由异常亚极光flows-created离子漂移(ASAID)和或SAPS-as复杂说equatorward-poleward ASAID-SAID或SAPS-ASAID。极光区,我们识别大在极光极光出现起伏区。波,结构化或复杂subauroral流动极光起伏大,和当地的地磁场振动确认subauroral流和连接极光与k - h波通过起伏不定近地的本征频率等离子体单(棉结)由k - h波谐振器激活。我们第一次演示同步检测磁层和附近的k - h波表面波等离子体层顶附近的热区7月16日,2017年,他们的结束通过棉结耦合谐振器的本征频率。因此,表面波等离子体层顶附近起伏的表现(或波及)向地球内部边界的棉结导致ASAID-SAID / SAPS-ASAID或发展SAPS-WS subauroral地区和大在极光区极光波动。

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