论文标题
主动重新连接的磁通传输鉴定:地球磁层中的MMS观测值
Magnetic Flux Transport Identification of Active Reconnection: MMS Observations in Earth's Magnetosphere
论文作者
论文摘要
磁重新连接在转换能量时起着重要作用,同时修改场拓扑。该过程发生在各种的等离子体环境中,其中磁通量的运输是固有的。在原位观测中识别主动磁重新连接位点具有挑战性。最近已经开发了一种新技术,即磁通传输(MFT)分析,并在数值模拟中得到了证明,可有效,准确地识别主动重新连接。在这项研究中,我们使用磁层多层测量值检查了37个先前报道的电子扩散区域(EDR)/重新连接线交叉事件的MFT过程。在X点上并存向内和向外的MFT流动提供了一个签名,即磁场线已断开和重新连接。 MFT分析在原位观察结果中的应用表明,MFT可以在复杂的各种条件下成功识别主动重新连接位点,包括不对称和湍流上游条件。它还提供了比单独的等离子体流出喷气机更高的识别率。 MFT可以应用于单飞行器任务和实验室实验的原位测量。
Magnetic reconnection plays an important role in converting energy while modifying field topology. This process takes place in varied plasma environments in which the transport of magnetic flux is intrinsic. Identifying active magnetic reconnection sites in in-situ observations is challenging. A new technique, Magnetic Flux Transport (MFT) analysis, has been developed recently and proven in numerical simulation for identifying active reconnection efficiently and accurately. In this study, we examine the MFT process in 37 previously reported electron diffusion region (EDR)/reconnection-line crossing events at the dayside magnetopause and in the magnetotail and turbulent magnetosheath using Magnetospheric Multiscale measurements. The coexisting inward and outward MFT flows at an X-point provides a signature that magnetic field lines become disconnected and reconnected. The application of MFT analysis to in-situ observations demonstrates that MFT can successfully identify active reconnection sites under complex varied conditions, including asymmetric and turbulent upstream conditions. It also provides a higher rate of identification than plasma outflow jets alone. MFT can be applied to in situ measurements from both single- and multi-spacecraft missions and laboratory experiments.