The magnetospheric response to a two-stream solar wind interval during solar maximum: a self-consistent magnetospheric model

Computer Science

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Solar Wind, Interplanetary Coronal Mass Ejections

Scientific paper

A two-stream solar wind interval (two interplanetary CME events) during 1-7 May 1998 is examined and the magnetospheric response to these events is modeled and compared to satellite data. The solar ejecta (CMEs) and resultant fast interplanetary streams cause magnetic storms with minimum Dst values of -75 nT and -205 nT, respectively. For the second, more intense magnetic storm, it is found that at the Earth's surface the maximum values of the disturbance fields are -208 nT for the ring current contribution (DR), 112 nT for the Chapman-Ferraro (DCF) magnetopause current system, and -161 nT for the tail current system (DT). Although DT is large, it is counterbalanced by DCF. These currents significantly modify the magnetospheric geometry and size and must be included for any accurate magnetic field representation during storm periods.

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