The conditions responsible for truncated forms of the Dst variation

Computer Science

Scientific paper

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Earth Magnetosphere, Magnetic Disturbances, Magnetic Field Reconnection, Ring Currents, Solar Wind, Stochastic Processes, Interplanetary Magnetic Fields, Magnetosheath, Solar Activity

Scientific paper

It is shown that the classical form of the Dst variation of a
geomagnetic disturbance with a deep main phase requires sufficiently
large values of the southern (B sub ZS) component of the IMF. Weaker,
truncated form of the Dst variation arise in the case of relatively
small values of B sub ZS.

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