The dew formation rate depends on the amount of watervapor in the air; this amount is related to the absolutehumidity (i.e., the amount of gaseous molecules in the air)and the difference between the dew point and ambienttemperature. This notion is expressed by the relativehumidity (RH), which is defined as the amount of watervapor in the air at a given temperature with respect to themaximum amount of water vapor that the air can hold atthat same temperature.
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