Substorm phenomena are reviewed with emphasis on the magnetospheric so
urce region of the onset, on the morphology of the initial breakup and
subsequent activations, and on the variable character of individual s
ubstorms. We provide evidence that before the substorm onset and durin
g the following activations an intense, thin current sheet is formed a
t the interface between the quasi-dipolar and taillike magnetic field
regions. We infer that the initial breakup, the following multiple act
ivations, pseudobreakups, and other short-term activations during nons
ubstorm times are all similar in morphology and have the same formatio
n mechanism. We postulate that the elementary units of energy dissipat
ion, impulsive dissipation events, which are localized in space and ha
ve a short lifetime of similar to 1 min, are the manifestations of tai
l reconnection. We also emphasize the evidence that previous authors h
ave presented in favor of this time dependence and localization. On th
e basis of the above, we suggest that there are two basic magnetospher
ic processes responsible for energy storage and dissipation during bot
h substorm and nonsubstorm times: A global and slow quasi-static tail
reconfiguration responsible for the energy storage, and a sequence of
local, sporadic, short-term energy dissipation events. These competiti
ve processes can be observed most the time in some part of the plasma
sheet; their relative intensity determines the type of large-scale dyn
amic evolution. In this scenario, the various dynamical situations are
interpreted as variations in the balance between the two competing pr
ocesses.