Because of the importance of oscillatory components in the oncoming fl
ow at certain oceanic topographic features, we investigate the oscilla
tory flow past a circular cylinder in an homogeneous rotating fluid. W
hen the oncoming flow is non-reversing, and for relatively low-frequen
cy oscillations, the modifications to the equivalent steady flow arise
principally in the 'quarter layer' on the surface of the cylinder. An
incipient-separation criterion is found as a limitation on the magnit
ude of the Rossby number, as in the steady-flow case. We present exact
solutions for a number of asymptotic cases, at both large frequency a
nd small nonlinearity. We also report numerical solutions of the nonli
near quarter-layer equation for a range of parameters, obtained by a t
emporal integration. Year the rear stagnation point of the cylinder, w
e find a generalized velocity 'plateau' similar to that of the steady-
flow problem, in which all harmonics of the free-stream oscillation ma
y be present. Further, we determine that, for certain initial conditio
ns, the boundary-layer flow develops a finite-time singularity in the
neighbourhood of the rear stagnation point.