Comparative Analysis of the Vlasiator Simulations and MMS Observations of Multiple X-Line Reconnection and Flux Transfer Events

Autor: Mojtaba Akhavan-Tafti, D. J. Gershman, Julia E. Stawarz, Minna Palmroth, Urs Ganse, Maxime Grandin, Guan Le, Jonathan Eastwood, James A. Slavin, Markus Battarbee
Přispěvatelé: Department of Physics, Space Physics Research Group, Particle Physics and Astrophysics
Jazyk: angličtina
Rok vydání: 2020
Předmět:
MECHANISM
Informatics
010504 meteorology & atmospheric sciences
MOTION
MAGNETOPAUSE
01 natural sciences
global hybrid-Vlasov Vlasiator simulations
MAGNETIC RECONNECTION
Instruments and Techniques
Interplanetary magnetic field
Research Articles
Physics
Community Standards
PLASMA
reconnection-driven magnetic island dynamics
Planetary Magnetospheres
Magnetic flux
Geophysics
Magnetospheres
Physics::Space Physics
Magnetopause
Planetary Sciences: Comets and Small Bodies
Research Article
flux transfer events
114 Physical sciences
ELECTRON-DIFFUSION REGION
Physics::Plasma Physics
Electric field
0201 Astronomical and Space Sciences
FTE evolution
Results of the GEM Dayside Kinetics Southward IMF Challenge
MESSENGER OBSERVATIONS
Magnetospheric Physics
FIELD
Planetary Sciences: Solid Surface Planets
Planetary Sciences: Fluid Planets
0105 earth and related environmental sciences
Coalescence (physics)
Solar Physics
Astrophysics
and Astronomy

reconnection‐driven magnetic island dynamics
Magnetic reconnection
Plasma
115 Astronomy
Space science

Computational physics
Magnetospheric Multiscale Mission
Space and Planetary Science
global hybrid‐Vlasov Vlasiator simulations
Space Plasma Physics
0401 Atmospheric Sciences
Interactions with Solar Wind Plasma and Fields
Zdroj: Journal of Geophysical Research. Space Physics
Journal of Geophysical Research: Space Physics
Popis: The Vlasiator hybrid‐Vlasov code was developed to investigate global magnetospheric dynamics at ion‐kinetic scales. Here we focus on the role of magnetic reconnection in the formation and evolution of magnetic islands at the low‐latitude magnetopause, under southward interplanetary magnetic field conditions. The simulation results indicate that (1) the magnetic reconnection ion kinetics, including the Earthward pointing Larmor electric field on the magnetospheric side of an X‐point and anisotropic ion distributions, are well‐captured by Vlasiator, thus enabling the study of reconnection‐driven magnetic island evolution processes, (2) magnetic islands evolve due to continuous reconnection at adjacent X‐points, “coalescence” which refers to the merging of neighboring islands to create a larger island, “erosion” during which an island loses magnetic flux due to reconnection, and “division” which involves the splitting of an island into smaller islands, and (3) continuous reconnection at adjacent X‐points is the dominant source of magnetic flux and plasma to the outer layers of magnetic islands resulting in cross‐sectional growth rates up to + 0.3 RE 2/min. The simulation results are compared to the Magnetospheric Multiscale (MMS) measurements of a chain of ion‐scale flux transfer events (FTEs) sandwiched between two dominant X‐lines. The MMS measurements similarly reveal (1) anisotropic ion populations and (2) normalized reconnection rate ~0.18, in agreement with theory and the Vlasiator predictions. Based on the simulation results and the MMS measurements, it is estimated that the observed ion‐scale FTEs may grow Earth‐sized within ~10 min, which is comparable to the average transport time for FTEs formed in the subsolar region to the high‐latitude magnetopause. Future simulations shall revisit reconnection‐driven island evolution processes with improved spatial resolutions.
Key Points Anisotropic ion distributions are reported in Vlasiator simulations and MMS observations of reconnection inflow regionsThe 2‐D simulations suggest magnetic islands grow mainly via continuous reconnection. Island coalescence, erosion, and division are also presentBased on simulation results, ion‐scale FTEs are estimated to grow at
Databáze: OpenAIRE