The fundamental problem of thermoacoustic streaming on a rigid sphere in a
strong standing acoustic field has been treated analytically. The sphere ra
dius (a) is taken to be large compared with the displacement amplitude (A)
of fluid oscillations, and yet small on the scale of the radian wavelength
(lambda/2 pi) of the sound field. Only the high frequency limit is consider
ed here, for which the Stokes oscillatory boundary layer thickness (delta(n
u)) is much smaller than the sphere radius (a), and the streaming effects i
n the boundary layer are most pronounced. It is found that the phased inter
action of the first-order harmonic quantities in the boundary layer is capa
ble of introducing a second-order time-averaged temperature distribution, i
n addition to the well-known second-order time-averaged fluid motion. The a
ssociated steady temperature gradients cause localized heating and cooling
variations over the surface of the sphere, whose net result is always a mea
n heating of the sphere. The role of little-known second-order thermodynami
c moduli is pointed out, which, however, do not contribute to this phenomen
on for the case of an ideal gas host fluid. Results for this time-averaged
thermal effect are presented and discussed with reference to a possible nov
el application to the acoustic heating of small particles using ultrasonic
frequencies for which heat fluxes of O(1) kW m(-2) can be achieved.