Electron magnetic reconnection without ion coupling in Earth’s turbulent magnetosheath
- Univ. of California, Berkeley, CA (United States)
- Imperial College, London (United Kingdom)
- Univ. of Delaware, Newark, DE (United States)
- Univ. of Maryland, College Park, MD (United States)
- Dartmouth College, Hanover, NH (United States)
- ISAS/JAXA, Sagamihara (Japan)
- West Virginia Univ., Morgantown, WV (United States)
- Southwest Research Inst. (SwRI), San Antonio, TX (United States)
- Univ. of New Hampshire, Durham, NH (United States)
- The Catholic Univ. of America, Washington, DC (United States); NASA Goddard Space Flight Center (GSFC), Greenbelt, MD (United States)
- NASA Goddard Space Flight Center (GSFC), Greenbelt, MD (United States)
- Denali Scientific, Healy, AK (United States)
- Swedish Inst. of Space Physics, Uppsala (Sweden)
- Univ. de Toulouse (France)
- Univ. of Colorado, Boulder, CO (United States)
- Ecole Polytechnique, Paris(France)
- Univ. of California, Los Angeles, CA (United States)
- KTH Royal Inst. of Technology, Stockholm (Sweden)
- Austrian Academy of Sciences, Graz (Austria)
Magnetic reconnection in current sheets is a magnetic-to-particle energy conversion process that is fundamental to many space and laboratory plasma systems. In the standard model of reconnection, this process occurs in a minuscule electron-scale diffusion region. On larger scales, ions couple to the newly reconnected magnetic-field lines and are ejected away from the diffusion region in the form of bi-directional ion jets at the ion Alfvén speed. Much of the energy conversion occurs in spatially extended ion exhausts downstream of the diffusion region. In turbulent plasmas, which contain a large number of small-scale current sheets, reconnection has long been suggested to have a major role in the dissipation of turbulent energy at kinetic scales. However, evidence for reconnection plasma jetting in small-scale turbulent plasmas has so far been lacking. Here we report observations made in Earth’s turbulent magnetosheath region (downstream of the bow shock) of an electron-scale current sheet in which diverging bi-directional super-ion-Alfvénic electron jets, parallel electric fields and enhanced magnetic-to-particle energy conversion were detected. Contrary to the standard model of reconnection, the thin reconnecting current sheet was not embedded in a wider ion-scale current layer and no ion jets were detected. Observations of this and other similar, but unidirectional, electron jet events without signatures of ion reconnection reveal a form of reconnection that can drive turbulent energy transfer and dissipation in electron-scale current sheets without ion coupling.
- Research Organization:
- Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States). National Energy Research Scientific Computing Center (NERSC)
- Sponsoring Organization:
- USDOE
- OSTI ID:
- 1543769
- Journal Information:
- Nature (London), Vol. 557, Issue 7704; ISSN 0028-0836
- Publisher:
- Nature Publishing GroupCopyright Statement
- Country of Publication:
- United States
- Language:
- English
Web of Science
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