Identifying Magnetotail Jet Front Signatures in a 3D + 3V Global Hybrid-Vlasov Simulation

IF 2.6 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS
L. Pänkäläinen, G. Cozzani, M. Battarbee, U. Ganse, Y. Pfau-Kempf, J. Suni, M. Palmroth
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Abstract

Magnetic reconnection in Earth's magnetotail is thought to create bursty bulk flows (BBFs), short-lived plasma bulk velocity enhancements in the magnetotail's central plasma sheet (CPS) region. Closely related to BBFs are dipolarization fronts (DFs), sudden increases in B z ${B}_{z}$ , the magnetic field component aligned with Earth's magnetic dipole axis. BBFs are involved in, for example, transport of energy and mass, and DFs contribute to for instance energy conversion processes and plasma acceleration. Both phenomena increase magnetic flux transport in the magnetotail. We demonstrate novel methods of identifying BBFs and DFs in 3D global magnetospheric simulations and present results for multiple case studies. We search for BBFs and DFs in a simulation conducted using the 3D global magnetospheric hybrid-Vlasov code Vlasiator. DFs are identified using a B z ${B}_{z}$ time derivative threshold, whereas BBFs are defined based on a velocity threshold. The tailward DF (anti-DF) identification criteria are fulfilled by tailward-propagating flux ropes, while earthward-propagating DFs are mostly seen in finger-like structures of high earthward bulk velocity alongside BBFs. We show that detections of fast flows meeting the BBF criteria in virtual spacecraft time series also originate due to moving reconnection locations and movement of the current sheet within the CPS region, while the reconnection outflow stays roughly constant. The results show that rapid B z ${B}_{z}$ variations in the simulation have multiple sources, and similar satellite measurements of BBFs can arise from different physical phenomena. Our findings may help with interpreting satellite observations in the magnetotail.

三维+ 3V全球混合vlasov仿真中磁尾射流前特征识别
地球磁尾中的磁重联被认为会产生突发体流(bbf),在磁尾中央等离子体片(CPS)区域短暂的等离子体体速度增强。与bbf密切相关的是双极化锋(DFs), B z ${B}_{z}$的突然增加,磁场分量与地球磁偶极子轴对齐。例如,bbf参与能量和质量的传输,而df有助于能量转换过程和等离子体加速。这两种现象都增加了磁尾中的磁通量输运。我们展示了在三维全球磁层模拟中识别bbf和df的新方法,并提供了多个案例研究的结果。我们在三维全球磁层混合vlasov代码Vlasiator进行的模拟中搜索bbf和df。使用bz ${B}_{z}$时间导数阈值识别df,而bbf是基于速度阈值定义的。尾向DF(反DF)识别标准是通过尾向传播通量绳来实现的,而向地传播DF主要出现在向地高体速的指状结构中。我们表明,在虚拟航天器时间序列中,满足BBF标准的快速流检测也源于CPS区域内重新连接位置的移动和电流片的移动,而重新连接流出量大致保持不变。结果表明,模拟中快速的bz ${B}_{z}$变化有多个来源,类似的bbf卫星测量可能来自不同的物理现象。我们的发现可能有助于解释磁尾中的卫星观测结果。
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来源期刊
Journal of Geophysical Research: Space Physics
Journal of Geophysical Research: Space Physics Earth and Planetary Sciences-Geophysics
CiteScore
5.30
自引率
35.70%
发文量
570
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