The remarkably strong radar echoes from the summer polar mesosphere ha
ve been an enigma to atmospheric and radar scientists since their disc
overy more than a decade ago. Since then, more sophisticated radar exp
eriments and in situ rocket measurements have shed some light on the u
nderlying physics and chemistry, and theories have been formulated to
explain the generation of the intense radar backscatter and the remark
able physical conditions associated with it. First, we review the key
observations and examine the proposed theories. We then evaluate the p
rogress that has been made in understanding this phenomenon and explor
e its connection to global change, to the newly recognized material re
ferred to as a dusty plasma, and to the highest clouds in the Earth's
atmosphere. Finally, we end with suggestions for future research.