Pj. Tackley, EFFECTS OF STRONGLY TEMPERATURE-DEPENDENT VISCOSITY ON TIME-DEPENDENT, 3-DIMENSIONAL MODELS OF MANTLE CONVECTION, Geophysical research letters, 20(20), 1993, pp. 2187-2190
Numerical simulations of thermal convection in a wide (8x8x1) Cartesia
n box heated from below with temperature-dependent viscosity contrasts
of 1000, and Rayleigh number 105 show that boundary conditions and as
pect ratio have an enormous effect on the preferred flow pattern. With
rigid upper and lower boundaries, spoke-pattern flow with small (diam
eter approximately 1.5) cells is obtained, consistent with laboratory
experiments and previous numerical results. However, with the arguably
more realistic stress-free boundaries, the flow chooses the largest p
ossible wavelength, forming a single square cell of aspect ratio 8, wi
th one huge cylindrical downwelling surrounded by upwelling sheets. Th
e addition of stress-dependence to the rheology weakens the stiff uppe
r boundary layer, resulting in smaller cells, though still with upwell
ing sheets and downwelling plumes.