The three-dimensional solar wind at solar activity minimum

In early 1998 the Ulysses spacecraft made history by completing an orbit ar ound the Sun inclined to the solar equator by 80 degrees. It observed the p roperties of the high-latitude heliosphere at a time of low solar activity when the configuration of the solar magnetic field was relatively simple. T he solar wind data acquired by Ulysses have placed firm observational const raints on theories of the acceleration of the fast wind from the polar regi ons. The speed of the polar solar wind was in the range 750-800 km s(-1), w ith a slow increase toward the poles. The polar proton flux of similar to 2 x 10(8) cm(-2) s(-1) was only two-thirds the low-latitude flux but still s ufficiently high to require energy sources in addition to the conduction of heat from the hot solar corona. In comparison with the slow, low-latitude solar wind, the heavy ions in the fast, high-latitude wind had less element al fractionation relative to the solar surface and a lower state of ionizat ion. Fine structures in the polar solar wind, named microstreams, exhibited a correlation between speed, proton temperature, and alpha particle abunda nce. The absence of a latitude dependence of the widths of the microstreams suggests that they are caused by temporal, rather than purely spatial vari ations at the Sun. Magnetic field observations revealed a latitude-independ ent radial field strength of similar to 3 nT (normalized to 1 AU) and a lar ge flux of outward propagating Alfven waves. The most probable direction of the interplanetary magnetic field was close to the Archimedes (Parker) spi ral predicted on the basis of radial fields close to the Sun combined with the effects of solar rotation. The fluctuations about the average direction were so large, however, that there was little latitudinal variation of the average value of \B-R\/B, where B-R is the radial component of the field w ith magnitude B. Latitudinal transport of field lines and nonradial field d irections near the Sun appear to be other necessary additions to the simple Parker model. Some unexpected differences were found between the low- and the high-latitude properties of the plasma from transient events called cor onal mass ejections (CMEs). At high latitudes, the speeds of the CME plasma clouds were close to the speed of the ambient fast wind, shocks were obser ved both ahead of and behind the CMEs, and enhancements of the helium abund ance and of high charge states of heavy ions were not observed, as they oft en are at low latitudes. The review closes with a summary of arguments in s upport of the view that the fast solar wind observed by Ulysses at intermed iate latitudes has its origin at higher latitudes in the polar coronal hole s.