Magnetic field measurements from the Ulysses space mission over the so
uth polar regions of the sun showed that the structure and properties
of the three-dimensional heliosphere were determined by the fast solar
wind flow and magnetic fields from the large coronal holes in the pol
ar regions of the sun. This conclusion applies at the current, minimum
phase of the 11-year solar activity cycle. Unexpectedly, the radial c
omponent of the magnetic field was independent of latitude. The high-l
atitude magnetic field deviated significantly from the expected Parker
geometry, probably because of large amplitude transverse fluctuations
. Low-frequency fluctuations had a high level of variance. The rate of
occurrence of discontinuities also increased significantly at high la
titudes.