An analysis is presented of the conjugate free convective heat transfer from a vertical, thermally thin n heated from above to the surrounding uid. An estimate is presented of the thermal penetration length over which the temperature of a very long n would decrease from its maximum value at the top to the ambient temperature of the uid. The solution of the problem is shown to depend on two nondimensional parameters: the Prandtl number of the uid and the ratio s of the thermal penetration length to the actual length of the n. The overall heat transfer rate for thermally short ns (large s) is practically independent of the n material, whereas it depends on the thermal conductivity of the n when s is small. Numerical and asymptotic results are given covering the whole range of s.
Nomenclaturetemperature gradient de ned in Eq. (51) g = gravity acceleration h = half-thicknessof the n L = length of the n L ¤ = thermal penetration length de ned in Eq. (1) Nu = Nusselt number de ned in Eq. (15) Pr = Prandtl number of the uid, º½C p =Q = total heat ux at the top of the n Ra ¤ = Rayleigh number, ½cg¯1T L ¤3 =¸º Ra h = Rayleigh number based on the half-thickness of the n Ra L = Rayleigh number based on the length of the n s = ratio of L ¤ to L T 0 = temperature at the top of the n T 1 = temperature of the uid far from the n U; V = nondimensional longitudinal and transverse velocity components, respectively, de ned in Eq. (39) x; y = Cartesian coordinates, longitudinal and transverse, respectively z = nondimensional transverse coordinate de ned in Eq. (39) = thermal expansion coef cient of uid " = aspect ratio of the n, h=L nondimensionaltransverse coordinate de ned in Eq. (8) µ = nondimensionaltemperature of uid de ned in Eq. (8) µ w = nondimensionaltemperature of the n de ned in Eq. (7) = thermal conductivity of uiḑ w = thermal conductivity of the n º = kinematic coef cient of viscosity of uid ½ = density of uid ¾ = nondimensionallongitudinal coordinate de ned in Eq. (39)  = nondimensionallongitudinal coordinate de ned in Eq. (7) à = stream function for uid