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We have measured the mean temperature profiles T̄(z) and the thermal layer thickness δₜₕ(x,y) at various horizontal positions on the lower plate of a cylindrical convection cell, using water as the working fluid. The Rayleigh number Ra in the experiment varied from 2×10⁸ to 2×10¹⁰. The normalized vertical temperature profiles measured at various positions x along the direction of large scale circulation and for the same Ra are found to be self-similar, once the vertical distance z is scaled by the respective thermal layer thickness δₜₕ(x,0). Whereas those measured at different Ra do not have a universal form. Our results further reveal that the thermal layer thickness δₜₕ varied significantly in the two directions measured---along the large-scale circulation $(x)$ and perpendicular to it $(y)$. We found that the scaling exponent of δₜₕ with Ra is a function of x (and possibly a function of y as well), i.e. δₜₕ~ Ra^-β(x). Moreover, our results suggest that the thermal layer will eventually become uniform at very high Rayleigh numbers.
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Lui et al. (1998) studied this question.
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