Steady-state acoustic streaming flow patterns have been observed durin
g the operation of a variety of resonant single-axis ultrasonic levita
tors in a gaseous environment and in-the 20-37 kHz frequency range. Li
ght sheet illumination and scattering from smoke particles have reveal
ed primary streaming flows which display different characteristics at
low and high sound pressure levels. Secondary macroscopic streaming ce
lls around levitated samples are superimposed on the primary streaming
flow pattern generated by the standing wave. These recorded flows are
quite reproducible, and are qualitatively the same for a variety of l
evitator physical geometries. An onset of flow instability can also be
recorded in nonisothermal systems, such as levitated spot-heated samp
les when the resonance conditions are not exactly Satisfied. A prelimi
nary qualitative interpretation of these experimental results-is prese
nted in terms of the superposition of three discrete sets of circulati
on cells operating an different spatial scales. These relevant length
scales are the acoustic wavelength, the levitated sample size, and fin
ally the acoustic boundary layer thickness. This approach fails, howev
er, to explain the streaming flow-field morphology around liquid drops
levitated on Earth. Observation of the interaction between the flows
cells and the levitated samples also suggests the existence of a stead
y-state torque induced by the streaming flows.