A debate of long standing concerns the role viscous interactions play in ma
gnetospheric dynamics. Is it minor or is it central to, e.g., drive the low
latitude boundary layer on closed field lines and account for the substant
ial level of wave activity seen on the flanks? Newer data and theoretical c
onsiderations leave little doubt that viscous coupling is important. The Ke
lvin-Helmholtz instability is a major protagonist in fostering momentum tra
nsfer. Closer studies of the state of the flank magnetosphere will help to
resolve the issue.