Tearing instability, flux ropes, and the kinetic current sheet kink instability in the Earth`s magnetotail: A three-dimensional perspective from particle simulations

In this paper the tail current sheet is shown to be unstable to the kinetic current sheet kink instability (or simply the kinetic kink instability) in the crosstail plane (y–z plane) and under similar conditions that drive the tearing instability in the noon-midnight meridional plane (x–z plane). The tail current sheet is assumed to be a thin Harris current sheet (ρi/Lc ∼ 1) with equal ion and electron temperature. The kinetic kink instability develops due to the bending of the tail current sheet and the resulting pressure imbalance. The development of the kinetic kink instability including its growth rate and resultant distortion of the current sheet, is first examined using two-dimensional electromagnetic particle simulations. The coupling between the kinetic kink and tearing instabilities is then investigated via three-dimensional electromagnetic particle simulations. The results show that the tearing instability and the kinetic kink instability occur on the same timescale as what we expected from the two-dimensional simulations and that the projection of the field lines in the x–z plane reproduces a standard plasmoid shape. However, the three-dimensional plasmoid produced by the tearing instability is shown to consist of a series of flux ropes where the magnetic field lines are tightly wound as they cross the center of the current sheet. The entry and exit points of the field lines of the flux ropes are displaced in the dawn-dusk direction. Twist and displacement of the magnetic field lines arise from the magnetic field component By generated by a plasma current due to the differential motion between electrons and ions. This current and the associated flux ropes result from intrinsic particle effects. The kinetic kink instability bends the current sheet and the flux ropes along the y direction and generates large-scale cross-tail wavy structures. The wave fronts may eventually collide, causing a total distortion of the current sheet configuration and strong electron heating, while the tearing accounts for most of the ion heating.

[1]  D. Baker,et al.  Observations of Energetic Electrons (E 200 keV) in the Earth's Magnetotail' Plasma Sheet and Fireball Observations , 1977 .

[2]  B. Tsurutani,et al.  The relationship between the IMF B(y) and the distant tail (150-238 Re) lobe and plasmasheet B(y) fields , 1984 .

[3]  N. T. Gladd,et al.  Lower-hybrid-drift instability in field reversed plasmas , 1980 .

[4]  N. T. Gladd,et al.  Lower-hybrid-drift wave turbulence in the distant magnetotail. Interim report , 1978 .

[5]  R. Winglee,et al.  Electron beam injection during active experiments: 1. Electromagnetic wave emissions , 1990 .

[6]  H. Karimabadi,et al.  Collisionless reconnection in a quasi‐neutral sheet near marginal stability , 1989 .

[7]  C. Russell,et al.  Current carriers in the near-earth cross-tail current sheet during substorm growth phase , 1990 .

[8]  Motohiko Tanaka,et al.  Simulations on lower hybrid drift instability and anomalous resistivity in the magnetic neutral sheet , 1981 .

[9]  W. Hughes,et al.  Observations of earthward and tailward propagating flux rope plasmoids: Expanding the plasmoid model of geomagnetic substorms , 1994 .

[10]  W. Zwingmann,et al.  Particle simulation of magnetic reconnection in the magnetotail configuration , 1990 .

[11]  G. Parks,et al.  Particle orbits in model current sheets with a nonzero By component , 1993 .

[12]  P. Pritchett,et al.  does ion tearing exist , 1991 .

[13]  D. Winske Current‐driven microinstabilities in a neutral sheet , 1981 .

[14]  Ashis Bhattacharjee,et al.  Collisionless tearing instability in magnetotail plasmas , 1990 .

[15]  P. Pritchett,et al.  Convection and the formation of thin current sheets in the near‐Earth plasma sheet , 1994 .

[16]  F. Coroniti On the tearing mode in quasi‐neutral sheets , 1980 .

[17]  A. Nishida Magnetospheric plasma physics. , 1982 .

[18]  J. Slavin,et al.  The distant magnetotail's response to a strong interplanetary magnetic field By - Twisting, flattening, and field line bending , 1985 .

[19]  E. W. Hones,et al.  Three‐dimensional computer modeling of dynamic reconnection in the geomagnetic tail , 1981 .

[20]  Kunihiko Watanabe,et al.  Formation of field-twisting flux tubes on the magnetopause and solar wind particle entry into the magnetosphere , 1986 .

[21]  P. Palmadesso,et al.  Tearing instability in an anisotropic neutral sheet , 1983 .

[22]  Lev M. Zelenyi,et al.  Regular and chaotic charged particle motion in magnetotaillike field reversals: 1. Basic theory of trapped motion , 1989 .

[23]  S. Antiochos,et al.  Secondary instability in three-dimensional magnetic reconnection , 1992 .

[24]  K. Schindler,et al.  A theory of the substorm mechanism , 1974 .

[25]  E. G. Harris On a plasma sheath separating regions of oppositely directed magnetic field , 1962 .

[26]  R. Morse,et al.  NUMERICAL SIMULATION OF THE WEIBEL INSTABILITY IN ONE AND TWO DIMENSIONS. , 1971 .

[27]  L. Zelenyi,et al.  Tearing instability in plasma configurations , 1976 .

[28]  B. Coppi,et al.  Dynamics of the Geomagnetic Tail , 1966 .

[29]  Dan Winske,et al.  A cross‐field current instability for substorm expansions , 1991 .

[30]  J. Birn Computer studies of the dynamic evolution of the geomagnetic tail , 1980 .

[31]  R. Walker,et al.  A magnetohydrodynamic simulation of the formation of magnetic flux tubes at the earth's dayside magnetopause , 1989 .

[32]  A. Roux Generation of field-aligned current structures at substorm onsets , 1985 .

[33]  R. Walker,et al.  Magnetic flux ropes in 3-dimensional MHD simulations , 1990 .

[34]  E. W. Hones,et al.  The possible role of ionospheric oxygen in the initiation and development of plasma sheet instabilities , 1982 .

[35]  C. W. Allen,et al.  Interaction of the plasma sheet with the lobes of the Earth's magnetotail , 1987 .

[36]  K. Papadopoulos,et al.  A current disruption mechanism in the neutral sheet: A possible trigger for substorm expansions , 1990 .

[37]  C. Russell,et al.  ISEE‐1 and 2 observations of magnetic flux ropes in the magnetotail: FTE's in the plasma sheet? , 1986 .

[38]  R. Winglee,et al.  Energy storage and dissipation in the magnetotail during substorms 1. Particle simulations , 1993 .

[39]  J. Kan Developing a global model of magnetospheric substorms , 1990 .

[40]  P. Pritchett Effect of electron dynamics on collisionless reconnection in two-dimensional magnetotail equilibria , 1994 .

[41]  F. Coroniti Explosive tail reconnection: The growth and expansion phases of magnetospheric substorms , 1985 .

[42]  T. Engelder,et al.  Correction [to “An experimental study of permeability and fluid chemistry in an artificially jointed marble” by Chris Marone, James Rubenstone, and Terry Engelder] , 1989 .

[43]  R. Elphic,et al.  Current sheet thickness in the near-earth plasma sheet during substorm growth phase , 1990 .

[44]  René Pellat,et al.  Stability of a thick two‐dimensional quasineutral sheet , 1982 .

[45]  N. T. Gladd,et al.  On the role of the lower hybrid drift instability in substorm dynamics , 1981 .

[46]  Lev M. Zelenyi,et al.  Chaotization of the electron motion as the cause of an internal magnetotail instability and substorm onset , 1987 .

[47]  G. Paschmann,et al.  Average plasma properties in the central plasma sheet , 1989 .

[48]  Robert L. McPherron,et al.  Satellite studies of magnetospheric substorms on August 15, 1968. IX - Phenomenological model for substorms. , 1973 .

[49]  A. Langdon,et al.  Electromagnetic and Relativistic Plasma Simulation Models , 1976 .

[50]  Lou‐Chuang Lee,et al.  Streaming sausage, kink and tearing instabilities in a current sheet with applications to the earth's magnetotail , 1988 .