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A physical mechanism producing suprathermal populations and initiating substorms in the Earth's magnetotail

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Fig. 1. A 4-min interval showing Geotail data sets of day 247, 1997. From top to bottom, proton differential fluxes (58–77 keV), electron integral fluxes (E≥38 keV), B z (in nTs) and polar angle θ (in degrees) of the magnetic field, V x component of plasma
Fig. 2. Typical angular distributions for the 58–77 keV energetic proton fluxes of Fig
Fig. 3. A 5-min interval of day 247, 1997. Same format as in Fig. 1.
Fig. 4. A 15-min interval of day 68, 1995. Almost same format as in Fig. 1. The blue and red vertical dashed lines mark the highest proton and electron fluxes, respectively.
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