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C/NOFS measurements of ring current magnetic field in low-latitude ionosphere

机译:低纬度电离层中环电流磁场的C / NOFS测量

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The Vector Electric Field Instrument (VEFI) suite onboard the C/NOFS spacecraft includes a sensitive fluxgate magnetometer to measure DC and ULF magnetic fields in the low latitude ionosphere. The instrument includes a DC vector measurement at 1 sample/sec with a range of ± 45,000 nT whose primary objective is to enable both V × B and E × B measurements that are more accurate than those provided when a simple magnetic field model is used instead. The magnetic field data can also be used for scientific research to provide information of large-scale ionospheric and magnetospheric current systems. At low latitudes the magnetic field residuals (data with the internal magnetic field model subtracted) are predominately produced by the stormtime ring current. Since C/NOFS provides a complete coverage of all local times every 97 minutes, magnetic field data allow studies of the temporal evolution and local-time variations of stormtime ring current. The analysis demonstrates the feasibility of using instrumented spacecraft in low-inclination orbits to specify the ring current's evolution and local time asymmetry. We will present the results of a statistical study of the stormtime ring current.
机译:C / NOFS航天器的载体电磁场仪器(VEFI)套件包括一个敏感的磁通磁力计,用于测量低纬度电离层中的直流和ULF磁场。该仪器包括1个样本/秒的DC矢量测量,其主要目标是±45,000nt的范围,其主要目标是比使用简单磁场模型时提供的V×B和E×B的测量值更准确。磁场数据还可用于科学研究,以提供大型电离层和磁体电流系统的信息。在低纬度地区,磁场残差(减去内部磁场模型的数据)主要由Stormtime Ring电流产生。由于C / NOFS每97分钟提供所有当地时间的完整覆盖,磁场数据允许研究Stormtime Ring电流的时间演变和局部时间变化。分析表明,在低倾角轨道中使用仪表式航天器的可行性,以指定环电流的进化和局部时间不对称。我们将介绍Stormtime Ring Current的统计研究结果。

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