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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Global MHD simulation of flux transfer events at the high-latitude magnetopause observed by the Cluster spacecraft and the SuperDARN radar system
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Global MHD simulation of flux transfer events at the high-latitude magnetopause observed by the Cluster spacecraft and the SuperDARN radar system

机译:集群航天器和SuperDARN雷达系统观测到的高纬度磁更年期通量传输事件的全球MHD模拟

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A global magnetohydrodynamic numerical simulation is used to study the large-scale structure and formation location of flux transfer events (FTEs) in synergy with in situ spacecraft and ground-based observations. During the main period of interest on the 14 February 2001 from 0930 to 1100 UT the Cluster spacecraft were approaching the Northern Hemisphere high-latitude magnetopause in the postnoon sector on an outbound trajectory. Throughout this period the magnetic field, electron, and ion sensors on board Cluster observed characteristic signatures of FTEs. A few minutes delayed to these observations the Super Dual Auroral Radar Network (SuperDARN) system indicated flow disturbances in the conjugate ionospheres. These “two-point” observations on the ground and in space were closely correlated and were caused by ongoing unsteady reconnection in the vicinity of the spacecraft. The three-dimensional structures and dynamics of the observed FTEs and the associated reconnection sites are studied by using the Block-Adaptive-Tree-Solarwind-Roe-Upwind-Scheme (BATS-R-US) MHD code in combination with a simple open flux tube motion model (Cooling). Using these two models the spatial and temporal evolution of the FTEs is estimated. The models fill the gaps left by measurements and allow a “point-to-point” mapping between the instruments in order to investigate the global structure of the phenomenon. The modeled results presented are in good correlation with previous theoretical and observational studies addressing individual features of FTEs.
机译:全球磁流体动力学数值模拟用于与原位航天器和地面观测的协同作用来研究通量传递事件(FTE)的大规模结构和形成位置。在2001年2月14日从0930到1100 UT的主要关注时期,集束航天器以出轨轨迹接近午后的北半球高纬度磁更年期。在此期间,集群板上的磁场,电子和离子传感器观察到FTE的特征标记。这些观测结果延迟了几分钟,超级双极光雷达网络(SuperDARN)系统显示了共轭电离层中的流动扰动。这些在地面和太空中的“两点”观测是密切相关的,并且是由于航天器附近持续的不稳定重新连接造成的。通过使用块自适应树-风向-风向-上风方案(BATS-R-US)MHD代码结合简单的开放通量来研究观测到的FTE的三维结构和动力学以及相关的重新连接位置管运动模型(冷却)。使用这两个模型,可以估计FTE的时空演变。这些模型填补了测量留下的空白,并允许在仪器之间进行“点对点”映射,以调查现象的整体结构。提出的建模结果与针对FTE各个特征的先前理论和观察研究高度相关。

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