I want to measure boiling heat transfer of water from a hot solid surface at atmospheric conditions (exposed to surrounding air at constant pressure). Right now I'm determining which parameters to control in the experiment to obtain reproducible results.
For evaporation of water below its boiling point, it's important to take into account the relative humidity and temperature of the surrounding air. These determine the driving force for evaporation.
But for water above it's boiling point, the atmospheric conditions seem irrelevant, because water can continue to evaporate from the hot solid surface, even against its own pure vapor. It seems that whether the surrounding gas would be dry air, saturated air, or helium for that matter, the same results will be obtained. Is this reasoning correct?