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Investigation of Kinetic Ballooning Instability in 2D Harris Sheet Equilibrium with Finite Normal BZ Field.
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Substorm onset is believed to be a fundamental process for magnetic and
plasma energy transport in both magnetosphere and ionosphere.Ballooning
instability is one of the key trigger mechanism to examine the substorm
onset scenario in the near-Earth plasma sheet. For this subject,the
kinetic ballooning instability (KBI) in the near-Earth magnetotail is
analyzed using the general type of two-dimensional (2D) kinetic sheet
equilibria, the so-called generalized Harris sheet equilibria. The
kinetic ballooning mode is unstable in the intermediate range of
perpendicular wave number (ky) and the equatorial beta (eq). The growth
rate of the ballooning mode reduces signicantly with the increase in
electron and ion temperatures ratio (Te=Ti) and wave number ky. The
kinetic ballooning mode is found to be most unstable in the thin current
sheet region at the equatorial location xe ~(9-10)RE,
where the ballooning drive term (βeq/LpRc) is dominant on stiffening
effect due to the minimum in the normal magnetic field Bz there.Because
of the stabilizing effect through the field line stiffening factor and
the strong field line stabilization, the ballooning mode is stable close
to the Earth and becomes marginally unstable away from the Earth. This
suggests the local current sheet thinning may be also an effective
trigger mechanism for the onset of ballooning instability in the
near-Earth magnetotail.
Title: Investigation of Kinetic Ballooning Instability in 2D Harris Sheet Equilibrium with Finite Normal BZ Field.
Description:
Substorm onset is believed to be a fundamental process for magnetic and
plasma energy transport in both magnetosphere and ionosphere.
Ballooning
instability is one of the key trigger mechanism to examine the substorm
onset scenario in the near-Earth plasma sheet.
For this subject,the
kinetic ballooning instability (KBI) in the near-Earth magnetotail is
analyzed using the general type of two-dimensional (2D) kinetic sheet
equilibria, the so-called generalized Harris sheet equilibria.
The
kinetic ballooning mode is unstable in the intermediate range of
perpendicular wave number (ky) and the equatorial beta (eq).
The growth
rate of the ballooning mode reduces signicantly with the increase in
electron and ion temperatures ratio (Te=Ti) and wave number ky.
The
kinetic ballooning mode is found to be most unstable in the thin current
sheet region at the equatorial location xe ~(9-10)RE,
where the ballooning drive term (βeq/LpRc) is dominant on stiffening
effect due to the minimum in the normal magnetic field Bz there.
Because
of the stabilizing effect through the field line stiffening factor and
the strong field line stabilization, the ballooning mode is stable close
to the Earth and becomes marginally unstable away from the Earth.
This
suggests the local current sheet thinning may be also an effective
trigger mechanism for the onset of ballooning instability in the
near-Earth magnetotail.
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