Dew Point
Dew point temperature (Tdp) is the temperature at which moist air becomes saturated and water begins to condense if the air is cooled (at essentially constant pressure) without changing its moisture content.
Why dew point is useful
- Condensation risk: if a surface temperature drops below the air dew point, condensation is likely.
- Moisture “absolute” intuition: RH depends on temperature; dew point correlates more directly with the actual moisture content.
- HVAC processes: cooling and dehumidification lines on a psychrometric chart are often reasoned about using dew point and saturation.
How it relates to RH
At a fixed dry-bulb temperature, higher RH implies a higher dew point. If dew point is close to dry-bulb temperature, the air is near saturation. If dew point is much lower, the air is comparatively dry.
Common pitfalls
- Temperature vs moisture content: RH can change even if moisture content stays constant (because saturation pressure changes with temperature). Dew point helps avoid that confusion.
- Pressure/altitude: psychrometric properties depend on pressure. For best accuracy, use the correct site pressure or altitude.
- Measurement location: sensors exposed to radiant cooling or localized airflow can report misleading T/RH, affecting computed dew point.
Using FluidTool
In the humid air tool, set inputs such as Tdb + RH and read the computed Tdp. If you already know dew point and temperature, you can also use Tdb + Tdp as inputs.