We discuss an example of confinement of fast solar electrons by a disc
rete solar wind-interplanetary magnetic field structure on February 22
, 1991. The structure is about 190,000 km in width and is clearly defi
ned by changes in the direction of the magnetic field at the Ulysses s
pacecraft. This structure carries electrons moving toward the Sun as w
ell as away from the Sun. A loss cone in the angular distribution of t
he fast electrons shows that mirroring, presumably magnetic, tal;es pl
ace downstream from the spacecraft. Following passage of this narrow s
tructure, the return flux vanishes for 21 mill after which time the mi
rroring resumes and persists for several hours. We identify the enhanc
ed magnetic field region lying downstream from the Ulysses spacecraft
that is responsible for the mirroring to be a corotating stream intera
ction region. Backstreaming suprathermal electron measurements by the
Los Alamos National Laboratory plasma experiment on the Ulysses spacec
raft support this interpretation.