The relationship of flow field saddles to the formation of asymmetric
vortices is studied by employing a conical Navier-Stokes equation solv
er. Local grid resolution studies were used to demonstrate the importa
nce of capturing the leeside saddle point and the secondary separation
and reattachment points. The transient solutions from the unconverged
symmetric flow to the converged symmetric Bow illustrate a saddle poi
nt shift mechanism providing an explanation for the necessity of adequ
ate grid resolution in this region. Also studied were the paths and fi
nal solutions obtained with perturbed and unperturbed local time-stepp
ing procedures, and a perturbed time accurate method. The results indi
cate that the final solutions are virtually identical and that the sam
e general transient paths are followed. However, these paths are not i
dentical to those obtained with a quasi-steady pitch up of the cone in
which an abrupt shift from symmetric to asymmetric results occurs. Fi
nally, the qualitative accuracy of the conical results is assessed by
comparisons of the spherical cap streamlines with experimental results
of Lowson and Ponton. Excellent agreement is obtained for the inciden
ce ratios at which symmetric vortices are formed, a saddle point appea
rs and when vortex asymmetry occurs, although the solver does not comp
ute accurately the higher incidence hows which were reported to be non
-conical in the experiments. The quasi-steady pitch up cases also show
ed remarkable qualitative similarity to the experimental data. (C) 199
7 Elsevier Science Ltd.