The equilibrium vapor pressure of water over a liquid surface in moist air (\(p^*_{H_2O,a}\)) is slightly greater than the equilibrium vapor pressure over a pure water surface (\(p^*_{H_2O}\)). This difference is quantified by the water vapor enhancement factor, \(f_w\), which depends on temperature and the pressure of the moist air. The relationship is \(p^*_{H_2O,a} = f_w(T, p_{ms}) \cdot p^*_{H_2O}\).





