Abstract
Observations in Earth’s turbulent magnetosheath downstream of a quasiparallel bow shock reveal a prevalence of electron-scale current sheets favorable for electron-only reconnection where ions are not coupled to the reconnecting magnetic fields. In small-scale turbulence, magnetic structures associated with intense current sheets are limited in all dimensions. And since the coupling of ions are constrained by a minimum length scale, the dynamics of electron reconnection is likely to be 3D. Here, both 2D and 3D kinetic particle-in-cell simulations are used to investigate electron-only reconnection, focusing on the reconnection rate and associated electron flows. A new form of 3D electron-only reconnection spontaneously develops where the magnetic X-line is localized in the out-of-plane () direction. The consequence is an enhancement of the reconnection rate compared with two dimensions, which results from differential mass flux out of the diffusion region along , enabling a faster inflow velocity and thus a larger reconnection rate. This outflow along is due to the magnetic tension force in just as the conventional exhaust tension force, allowing particles to leave the diffusion region efficiently along unlike the 2D configuration.
- Received 30 March 2021
- Accepted 13 September 2021
DOI:https://doi.org/10.1103/PhysRevLett.127.155101
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