EGU2020-2848, updated on 08 Jan 2024
https://doi.org/10.5194/egusphere-egu2020-2848
EGU General Assembly 2020
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Disturbance of the front region of magnetic reconnection outflow jets due to the lower-hybrid drift instability

Takuma Nakamura1, Takayuki Umeda2, Rumi Nakamura1, Huishan Fu3, and Mitsuo Oka4
Takuma Nakamura et al.
  • 1Space Research Institute (IWF) / Austrian Academy of Sciences, Graz, Austria (takuma.tkm.nakamura@gmail.com)
  • 2Institute for Space-Earth Environmental Research (ISEE), Nagoya University
  • 3School of Space and Environment, Beihang University
  • 4Space Sciences Laboratory, University of California, Berkeley

Magnetic reconnection is a key process in collisionless plasmas that converts magnetic energy to plasma kinetic energies through changes in the magnetic field topology. The energy conversion in this process is believed to cause various explosive phenomena in space such as auroral substorms in the Earth’s magnetosphere and solar flares. Here, a 3D fully kinetic simulation shows that the lower-hybrid drift instability (LHDI) disturbs the front of magnetic reconnection outflow jets and additionally causes the energy dissipation. The peak energy dissipation at the jet fronts is comparable to the values seen near the center of the reconnection region where the topology change during reconnection occurs, indicating that the LHDI turbulence has a substantial effect on the energetics of reconnection. The result is well consistent with a disturbance observed at the dipolarization front (DF) in the Earth’s magnetotail by the Magnetospheric Multiscale (MMS) mission. A fully kinetic dispersion relation solver, validated by the MMS observations, further predicts that the disturbance of the reconnection jet front could occur over different parameter regimes in space plasmas including the Earth’s DF and solar flares.

How to cite: Nakamura, T., Umeda, T., Nakamura, R., Fu, H., and Oka, M.: Disturbance of the front region of magnetic reconnection outflow jets due to the lower-hybrid drift instability, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2848, https://doi.org/10.5194/egusphere-egu2020-2848, 2020.

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