Non-Oberbeck-Boussinesq effects in near-freezing water lower mean temperature, break mean-profile symmetry, shift critical Rayleigh number slightly, and preserve classical Nu and Re scalings after correction at intermediate Prandtl number.
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Non-Oberbeck-Boussinesq effects in coldwater
Non-Oberbeck-Boussinesq effects in near-freezing water lower mean temperature, break mean-profile symmetry, shift critical Rayleigh number slightly, and preserve classical Nu and Re scalings after correction at intermediate Prandtl number.