“…Similarity arguments (Landau & Lifshitz, 1987) for free convection suggest that we write the stream function as ψ(x, y) = ψ* (x/H, y/H, G, P), where G = g(T s -T 0R )H 3 / 2 and P = / are the Grashof and Prandtl numbers, respectively, and T s is a temperature characteristic of the surface. In addition, since we anticipate the surface temperatures to be close to uniform, except in the vicinity of x = 0 (Miyamoto et al, 1980;Pozzi & Lupo, 1988;Vynnycky & Kimura, 1996), we further specify the stream function to have the form (y > 0)…”