In May, 1993, the heliospheric current sheet (HCS) ceased to be seen b
y the Ulysses spacecraft at a heliocentric latitude of approximately 3
0-degrees-S and distance of 4.7 AU. The disappearance of the HCS coinc
ided with the solar wind speed remaining >560 km/s and with the disapp
earance of one of four interaction regions previously seen on each sol
ar rotation. The heliographic latitude of the disappearance of die HCS
at Ulysses was 11-degrees equatorward of the latitude of the magnetic
neutral sheet computed at the source surface at 2.5 solar radii, and
it occurred a half year earlier than predicted on the basis of the per
sistence of the time profile of the neutral sheet tilt from one solar
cycle to the next.