The separated flow past a zero-thickness flat plate held normal to a f
ree stream at Re=250 has been investigated through numerical experimen
ts. The long-time signatures of the drag and lift coefficients clearly
capture a low-frequency unsteadiness with a period of approximately 1
0 times the primary shedding period. The amplitude and frequency of dr
ag and lift variations during the shedding process are strongly modula
ted by the low frequency. A physical interpretation of the low-frequen
cy behaviour is that the flow gradually varies between two different r
egimes: a regime H of high mean drag and a regime L of low mean drag.
It is observed that in regime H the shear layer rolls up closer to the
plate to form coherent spanwise vortices, while in regime L the shear
layer extends farther downstream and the rolled-up Karman vortices ar
e less coherent. In the high-drag regime three-dimensionality is chara
cterized by coherent Karman vortices and reasonably well-organized str
eamwise vortices connecting the Karman vortices. With a non-dimensiona
l spanwise wavelength of about 1.2, the three-dimensionality in this r
egime is reminiscent of mode-B three-dimensionality. It is observed th
at the high degree of spanwise coherence that exists in regime H break
s down in regime L. Based on detailed numerical flow visualization we
conjecture that the formation of streamwise and spanwise vortices is n
ot in perfect synchronization and that the low-frequency unsteadiness
is the result of this imbalance (or phase mismatch).