Magnetospheric Multiscale Satellite Observations of Parallel Electron Acceleration in Magnetic Field Reconnection by Fermi Reflection from Time Domain Structures

被引:47
|
作者
Mozer, F. S. [1 ]
Agapitov, O. A. [1 ,2 ]
Artemyev, A. [3 ]
Burch, J. L. [4 ]
Ergun, R. E. [5 ]
Giles, B. L. [6 ]
Mourenas, D. [7 ]
Torbert, R. B. [8 ]
Phan, T. D. [1 ]
Vasko, I. [9 ]
机构
[1] Univ Calif Berkeley, Space Sci Lab, Berkeley, CA 94720 USA
[2] Taras Shevchenko Natl Univ Kyiv, Glushkova Ave 4, UA-01601 Kiev, Ukraine
[3] Univ Calif Los Angeles, Inst Geophys & Planetary Phys, Los Angeles, CA 90002 USA
[4] SW Res Inst, San Antonio, TX 78238 USA
[5] Univ Colorado, LASP, Boulder, CO 80303 USA
[6] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[7] Univ Orleans, E CNRS LPC2, F-45100 Orleans, France
[8] Univ New Hampshire, Durham, NH 03824 USA
[9] Russian Acad Sci, Space Res Inst, Moscow 117342, Russia
关键词
SOLITARY WAVES; MAGNETOTAIL; GEOTAIL; REGION; HOLES;
D O I
10.1103/PhysRevLett.116.145101
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
The same time domain structures (TDS) have been observed on two Magnetospheric Multiscale Satellites near Earth's dayside magnetopause. These TDS, traveling away from the X line along the magnetic field at 4000 km/s, accelerated field-aligned similar to 5 eV electrons to similar to 200 eV by a single Fermi reflection of the electrons by these overtaking barriers. Additionally, the TDS contained both positive and negative potentials, so they were a mixture of electron holes and double layers. They evolve in similar to 10 km of space or 7 ms of time and their spatial scale size is 10-20 km, which is much larger than the electron gyroradius (< 1 km) or the electron inertial length (4 km at the observation point, less nearer the X line).
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页数:5
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