Long-term enhancements in solar wind speed over timescales of the orde
r of a year appear to be a common feature throughout the heliosphere o
ver heliocentric distances that range from less than 0.72 AU to greate
r than 60 AU. The origin of these events remains to be determined, but
they are almost certainly associated with long-term variations st the
solar wind source, in contrast with smaller-scale structures such as
corotating interaction regions (CIRs), merged interaction regions (MIR
s), and global merged interaction regions (GMIRs), which are dynamical
in origin. We present a survey of the long-term speed enhancements ob
served at the Pioneer Venus Orbiter (PVO), IMP 8, Voyager 2, and Pione
er 10 between 1974 and 1994 and compare this with published reports of
smaller-scale events such as MIRs. We examine several of these long-t
erm speed enhancements in detail to identify and characterize aspects
of their structure, and then describe how that structure evolves with
heliocentric distance. Finally, we discuss some of the implications of
these events.