Magnetic field fluctuations during substorms.

Before a magnetospheric substorm and during its early phases, the magnetic field magnitude in the geomagnetic tail increases and field lines in the night-time hemisphere assume a more tail-like configuration. Before the substorm onset, a minimum amount of magnetic flux is observed to cross the neutral sheet which means that the neutral sheet currents attain their most earthward locations and their greatest current densities. This field configuration apparently results from an increased transport of magnetic flux to the tail caused by a southward interplanetary magnetic field. The field begins relaxing toward a more dipolar configuration at the time of a substorm onset with the recovery probably occurring first between 6 and 10 earth radii and later at greater distances. This recovery must be associated with magnetospheric convection which restores magnetic flux to the dayside hemisphere.