IntroductionCombined convection in rotating spherical annuli is of great interest in both engineering design and geophysics. The problem can be divided into two cases. The first is the case in which the gravitational field acts in radial direction and the second is that in which the gravitational field acts in the direction parallel to that of the axis of rotation. Although seemingly a minor change, the two problems are entirely different except in the forced convection limit. The former model is applicable to some geophysical or meteorological situations. The latter model is applicable to such physical flows as a rotating sphere viscometer (Bestman, 1978).In the past several studies concerning both cases were carried out. Pedlosky (1969) studied the steady motion of a thermally stratified fluid in a narrow spherical annulus with radial gravitational field. Douglass et al. (1978) obtained an approximate solution for the same problem using a modified Galerkin technique for moderate Reynolds numbers and several angular velocity ratios. The effects of different ratios of radii spheres on combined convection are shown in Douglass et al. (1979) in which a fourth order regular perturbation expansion method in powers of Reynolds number is used to solve the governing equations. A numerical investigation is performed by Raghavarao and Srinivas (1995a) for a similar problem using a parametric spline function approximation to solve the governing Navier Stokes and energy equations.An early study of combined convection flows in concentric spherical annulus with the gravitational field in axial direction is that of Riley and Mack (1972). They used a lower order perturbation expansion in powers of Reynolds number to obtain the approximate solution to the governing equations. Maples et al. (1973) studied the combined convection in spherical annulus experimentally. In their study only the inner sphere is allowed to rotate and Nusselt number