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Response of ionospheric convection to sharp southward IMF turnings inferred from magnetometer and radar data

机译:回应的电离层对流锋利国际货币基金组织(IMF)向南转向推断磁强计和雷达数据

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摘要

Reconfiguration of the convection pattern associated with a sudden transition in the north/south component of the IMF from stable positive to stable negative values is investigated for two events using both magnetometer and SuperDARN data. The IMF transition impinges upon the magnetosphere near the 10 MLT sector; perturbations are clearly seen on the dayside at the time of onset and on the nightside with a ~10 min delay from onset. This implies a dayside-to-nightside progression of the ionospheric response observed in the magnetic perturbations and SuperDARN velocities, contrary to the globally simultaneous response reported in the literature for a number of other events. The foci of the dawnside convection cells are shown to shift from near midnight toward the dayside, reaching a final location between 06 MLT and 08 MLT within 14-18 min of onset. The location of the duskside convection cell remains in the early afternoon sector both prior to and after the transition for both events. Once the convection foci reach a final location, the overall convection pattern enhances.
机译:重新配置的对流模式突然转变国际货币基金组织的北/南组件从稳定积极稳定的负值追究两个事件同时使用磁强计和SuperDARN数据。影响附近的磁气圈的过渡10 MLT部门;发病时的光面上阴面~ 10分钟延迟发作。意味着dayside-to-nightside进展的电离层响应中观察到磁扰动和SuperDARN速度,相反据全球同步响应文献的其他事件。疫源地的dawnside对流细胞所示从附近的午夜转向的光面,到达最终位置06 MLT和08年之间MLT 14 - 18分钟内发病。duskside对流细胞仍然在早期下午部门之前和之后过渡的事件。疫源地达成最后位置,整体提高对流模式。

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