K. Zhang et D. Gubbins, CONVECTION IN A ROTATING SPHERICAL FLUID SHELL WITH AN INHOMOGENEOUS TEMPERATURE BOUNDARY-CONDITION AT FINITE PRANDTL NUMBER, Physics of fluids, 8(5), 1996, pp. 1141-1148
We examine thermal convection in a rotating spherical shell with centr
al gravity and a spatially non-uniformly heated outer surface at two v
alues of the Prandtl number: P-r=7.0, appropriate for water at room te
mperature, and P-r=0.7, appropriate for air at standard temperature an
d pressure, by numerical calculation. Four calculations are performed
in a sequence: the onset of convection with homogeneous temperature bo
undary condition, nonlinear boundary-forced steady convection, stabili
ty of the forced steady convection to infinitesimal disturbances, and
time stepping of subsequent secondary convection. Unlike our previous
study of the infinite Prandtl number limit [J. Fluid Mech. 250, 209 (1
993)] inertial terms in the equation of motion for moderate Prandtl nu
mbers play a key role in the dynamics. The effects of an inhomogeneous
temperature boundary condition on nonlinear convection are illustrate
d by varying the wavelength and strength of the imposed boundary tempe
rature. It is shown that even a slight inhomogeneity in the thermal bo
undary condition can lock azimuthally drifting convection and make it
stationary, or modify the normal drifting convection rolls to a vacill
ating structure. In the infinite Prandtl number case, when inertial fo
rces are absent from the equation of motion, resonance occurs when the
wavelengths of boundary forcing and natural convection coincide. Flui
d inertia destroys this resonance for finite Prandtl number fluids. Th
e same effect reduces in size the stability region where steady convec
tion is locked to the boundary, and steady convection becomes unstable
to time-dependent convection. The period of the secondary convection
is close to that obtained with uniform temperature boundaries but the
spatial structure is dramatically changed, exhibiting vacillations bet
ween the wavelength of the boundary temperature and that of the natura
l convection. (C) 1996 American Institute of Physics.