Solar wind plasma observations made by the Ulysses spacecraft through
-80.2 degrees solar latitude and continuing equatorward to -40.1 degre
es are summarized. Recurrent high-speed streams and corotating interac
tion regions dominated at middle latitudes. The speed of the solar win
d was typically 700 to 800 kilometers per second poleward of -35 degre
es. Corotating reverse shocks persisted farther south than did forward
shocks because of the tilt of the heliomagnetic streamer belt. Sporad
ic coronal mass ejections were seen as far south as -60.5 degrees. Pro
ton temperature was higher and the electron strahl was broader at high
er latitudes. The high-latitude wind contained compressional, pressure
-balanced, and Alfvenic structures.