The Ulysses spacecraft passed through the Jovian system in February 19
92. Its trajectory, determined by its interplanetary mission, directed
the spacecraft to the previously unexplored high-latitude regions of
the Jovian magnetosphere. Like Pioneers 10 and 11 and the two Voyagers
, Ulysses entered the magnetosphere in the near equatorial morning sec
tor, but unlike the previous spacecraft, Ulysses exited at high latitu
de near local dusk. This report considerably extends the work of Lanze
rotti et al. (1993) by analyzing the extent of rotational anisotropy a
t high southern Jovigraphic latitudes attained by Ulysses during its o
utbound pass. Using data acquired by the Ulysses Heliosphere Instrumen
t for Spectral, Composition, and Anisotropy at Low Energies (HI-SCALE)
, we report some evidence of corotational flow in the high-latitude du
skside magnetosphere. On the inbound pass the Ulysses HI-SCALE instrum
ent observed anisotropies indicating partial corotation and a corotati
on lag. These data are consistent with Voyager plasma and energetic pa
rticle results. This is the first report of flow in the corotational d
irection from 44-57 R(J) in the duskside, high-latitude Jovian magneto
sphere. There is strong evidence for a substantially reduced corotatio
nal anisotropy in this duskside region relative to a comparable radial
distance range, 47-59 R(J), on the dayside.