Heat and Mass Transport
Dew-point temperature is the temperature at which air becomes saturated with moisture and water vapor begins to condense into liquid. This concept is critical in understanding humidity and condensation processes, as it indicates the point at which the air can no longer hold all of its moisture, leading to phenomena such as fog and dew formation. Recognizing the dew-point temperature helps in designing cooling systems and optimizing processes involving heat and mass transport.
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