Solar disturbances are observed to have significant effects in near-Earth s
pace. Over the past half-century of observation, a relatively clear picture
has developed of how and why the typical solar wind - as well as the most
extreme solar events - drive geospace responses. It is clear that magnetosp
heric substorms, geomagnetic storms (both recurrent and aperiodic events),
and even certain atmospheric chemical changes have their origins in the sol
ar-terrestrial coupling arena. High-speed solar wind streams and fast coron
al mass ejections (CMEs) can often have strong interplanetary shock waves a
nd southward magnetic fields which can initiate strong storm responses. We
demonstrate in this review that available modem space-observing platforms a
nd ground facilities allow us to trace drivers from the Sun to the Earth's
atmosphere. This allows us to assess quantitatively the energy transport th
at occurs throughout the Sun-Earth system during both typical and extreme c
onditions. Hence, we are continuously improving our understanding of "space
weather" and its effects on human society. (C) 2000 Elsevier Science Ltd.
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