Ulysses has frequently observed solar wind structures lasting from sev
eral hours to several days since it passed into the region of solar wi
nd emanating from the southern polar coronal hole at similar to 36 deg
rees S. In addition to previously reported Alfven waves and coronal ma
ss ejections, two other sorts of structures are routinely evident. Thi
s paper provides the first report of these structures in the high-lati
tude solar wind: (1) small-scale compressional structures and (2) pres
sure balance structures. The compressional structures are driven by fa
ster solar wind overtaking slower solar wind ahead of it and exhibit t
he plasma and field properties expected for compressions. Unlike large
-scale stream interaction regions observed in and near the ecliptic pl
ane, these structures are much smaller scale and are nonrecurring from
one rotation to the next. These smaller-scale compressional structure
s appear to arise preferentially from a limited (similar to 120 degree
s of heliolongitude) region in the southern polar coronal hole. The pr
essure balance structures, on the other hand, are indicated by roughly
equal increases in the plasma pressure and decreases in the magnetic
field pressure, These structures, which are several degrees across, ar
e more dense and have higher plasma pressures and betas than the surro
unding solar wind. These pressure balance structures may be the interp
lanetary manifestations of ''polar plumes.''