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Initial ionospheric observations made by the new Resolute incoherent scatter radar and comparison to solar wind IMF

机译:新型Resolute非相干散射雷达进行的初步电离层观测以及与太阳风IMF的比较

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摘要

The first Resolute incoherent scatter radar observations of the polar ionospheric F region show the fine control of the ionospheric plasma density and flow (electric field) by the solar wind interplanetary magnetic field (IMF). A summary of 8 days of observations is presented and 10 IMF B_z southward turning events during this period are analyzed in terms of the time delay of plasma density enhancements and ionospheric convection intensification with respect to the timing of B_z southward turning. We find that N_e enhancements are strongly tied to strong (?5 nT) IMF B _z southward turnings; arrive 25-75 mins (depending on MLT) after the IMF pulse arrives at the bowshock nose; last as long as B_z stays southward; contain as small as ~25 km horizontal substructures; are altitudinally smooth, a characteristic of a solar produced plasma. The most predictable response of ionospheric convection is anti-sunward flow intensification on average ~25 mins after B_z southward change.
机译:极地电离层F区域的第一批Resolute非相干散射雷达观测结果表明,太阳风行星际磁场(IMF)可以很好地控制电离层等离子体的密度和流量(电场)。给出了为期8天的观测结果的总结,并针对B_z向南转弯的时间,根据等离子体密度增强和电离层对流强化的时间延迟,分析了此期间的10个IMF B_z向南转弯事件。我们发现N_e增强与强大的(?5 nT)IMF B _z向南转弯紧密相关。在IMF脉冲到达弓形鼻后25-75分钟(取决于MLT);只要B_z一直向南,包含约25 km的水平子结构;高度光滑,这是太阳能产生的等离子体的特征。电离层对流最可预测的响应是B_z向南变化平均后约25分钟的反日流增强。

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