首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Plasma drifts and polarization electric fields associated with TID-like disturbances in the low-latitude ionosphere: C/NOFS observations
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Plasma drifts and polarization electric fields associated with TID-like disturbances in the low-latitude ionosphere: C/NOFS observations

机译:低纬度电离层中与TID样干扰相关的等离子体漂移和极化电场:C / NOFS观测

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Medium-scale traveling ionospheric disturbances are often observed at themagnetically conjugate points in the nighttime midlatitude ionosphere. It has been suggested that gravity waves disturb the ionosphere and induce electric fields in one hemisphere and that the electric fields are amplified by the Perkins instability and transmitted along the geomagnetic field lines to the conjugate ionosphere, creating similar disturbances there. However, direct observations of electric fields associated with traveling ionospheric disturbances (TIDs) are very few. In this study, we present low-latitude TID-like disturbances observed by the Communication/Navigation Outage Forecasting System (C/NOFS) satellite. It is found that ion velocity perturbations are generated in the directions parallel and perpendicular to the geomagnetic field within TIDs. Both the parallel and perpendicular ion velocity perturbations show an in-phase correlation with the ion density perturbations. For nighttime TIDs, the amplitude of both the parallel and meridional ion velocity perturbations increases almost linearly with the amplitude of the ion density perturbations, and the meridional ion drift is proportional to the parallel ion velocity. For daytime TIDs, the parallel ion velocity perturbation increases with the ion density perturbation, but themeridional ion velocity perturbation does not changemuch. The observations provide evidence that polarization electric field is generated within TIDs at low latitudes and maps along the geomagnetic field lines over a large distance.
机译:经常在夜间中纬度电离层的磁共轭点观测到中等规模的电离层扰动。已经提出,重力波扰动电离层并在一个半球内感应电场,并且该电场被珀金斯不稳定性放大并沿着地磁场线传输到共轭电离层,从而在那里产生类似的扰动。然而,与行进的电离层扰动(TID)相关的电场的直接观测很少。在这项研究中,我们介绍了由通信/导航中断预测系统(C / NOFS)卫星观测到的低纬度TID样干扰。发现离子速度扰动是在与TID内的地磁场平行和垂直的方向上产生的。平行和垂直离子速度扰动均显示与离子密度扰动同相相关。对于夜间TID,平行和子午离子速度扰动的幅度都几乎与离子密度扰动的幅度线性增加,而子午离子漂移与平行离子速度成正比。对于白天的TID,平行离子速度的扰动随离子密度的扰动而增加,而水平离子速度的扰动却没有太大变化。这些观察结果提供了证据,表明极化电场是在低纬度的TID内产生的,并沿着地磁场线在很长的距离上成图。

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