Abstract
Three flux ropes associated with near-Earth magnetotail reconnection are analyzed using Magnetospheric Multiscale observations. The flux ropes are Earthward propagating with sizes from ∼3 to 11 ion inertial lengths. Significantly different axial orientations are observed, suggesting spatiotemporal variability in the reconnection and/or flux rope dynamics. An electron-scale vortex, associated with one of the most intense electric fields (E) in the event, is observed within one of the flux ropes. This E is predominantly perpendicular to the magnetic field (B); the electron vortex is frozen-in with E × B drifting electrons carrying perpendicular current and causing a small-scale magnetic enhancement. The vortex is ∼16 electron gyroradii in size perpendicular to B and potentially elongated parallel to B. The need to decouple the frozen-in vortical motion from the surrounding plasma implies a parallel E at the structure's ends. The formation of frozen-in electron vortices within reconnection-generated flux ropes may have implications for particle acceleration.
| Original language | English |
|---|---|
| Pages (from-to) | 8783-8792 |
| Number of pages | 10 |
| Journal | Geophysical Research Letters |
| Volume | 45 |
| Issue number | 17 |
| DOIs | |
| Publication status | Published - 16 Sept 2018 |
Keywords
- Earth's magnetotail
- Magnetospheric Multiscale
- electron vortex
- flux ropes
- magnetic reconnection