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Features of the Solar Wind Plasma Flow around the Earth's Magnetosphere

机译:地球磁层周围的太阳风等离子体流动的特点

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The change in the properties of the solar wind flow as it crosses the bow shock wave front and moves in the Earth's magnetosheath are discussed. Solar wind data are used to study the refraction of magnetohydrodynamic (MHD) shock waves and the stationary tangential discontinuity of the solar wind into the magnetosheath. It is shown that the refraction of the solar-wind rotational discontinuity into the magnetosheath is accompanied by the emergence of a plateau-type plasma inhomogeneity with respect to the density of charged particles, with a simultaneous decrease in the magnetic field intensity. Moreover, the breaking of the secondary MHD contraction wave, reflected from the magnetopause, may be accompanied by the emergence of a fast reverse shock wave.
机译:讨论了太阳风流量的性质的变化,随着它穿过弓形冲击波前面并在地球磁性的移动中移动。 太阳能风数据用于研究磁性流动动力学(MHD)冲击波的折射以及太阳风的静态切线不连续性进入磁性。 结果表明,太阳风旋转不连续性进入磁性晶体晶片的折射伴随着相对于带电粒子的密度的高原型等离子体的出现,同时降低磁场强度。 此外,从磁档中反射的次级MHD收缩波的断开可以伴随快速逆向冲击波的出现。

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