Near the tail boundary beyond about 100 Re, GEOTAIL often measures irr
egular, long-period oscillations in plasma velocity and density. Flow
speed and density oscillate between magnetosheath values and values an
order of magnitude less. The oscillations can persist for days. A typ
ical oscillation lasts 100 minutes, but the range is large. The oscill
ations are highly asymmetric in that the increasing phase of the oscil
lation is an order of magnitude faster than the decreasing phase. This
asymmetry shows that they are a distinct class of oscillations, not p
reviously explicitly reported, and that they are not mere consequences
of tail flapping in a variable solar wind. The changes in flow direct
ion through an oscillation imply that the oscillation results from a m
otion of the boundary toward and away from the spacecraft with an ampl
itude between 5 and 10 R(e). A consideration of options suggests that
the most plausible cause of these oscillations is the 'breathing' of t
he magnetotail that attends the substorm cycle.