This paper gives analytical and numerical solutions for both westward
and eastward flows past obstacles on a beta-plane. The flows are consi
dered in the quasi-geostrophic limit where nonlinearity and viscosity
allow deviations from purely geostrophic flow. Asymptotic solutions fo
r the layer structure in almost-inviscid flow are given for westward f
low past both circular and more elongated cylindrical obstacles. Struc
tures are given for all strengths of nonlinearity from purely linear f
low through to strongly nonlinear flows where viscosity is negligible
and potential vorticity conserved. These structures are supported by a
ccurate numerical computations. Results on detraining nonlinear wester
n boundary layers and corner regions in Page & Johnson (1991) are used
to present the full structure for eastward flow past an obstacle with
a bluff rear face, completing previous analysis in Page & Johnson (19
90) of eastward flow past obstacles without rear stagnation points. Vi
scous separation is discussed and analytical structures proposed for s
eparated flows. These lead to predictions for the size of separated re
gions that reproduce the behaviour observed in experiments and numeric
al computations on beta-plane flows.