RH vs Humidity Ratio (W)
Relative humidity (RH) and humidity ratio (W) both describe moisture in air, but they answer different questions. Mixing them up is one of the most common psychrometrics mistakes in HVAC.
Two different “moisture” concepts
“How close am I to saturation at this temperature?” RH is a ratio to the saturation limit, so it changes when temperature changes.
“How much water vapor do I actually have?” W is an absolute moisture measure (mass of water vapor per mass of dry air). It stays nearly constant when air is heated or cooled without adding/removing moisture (at roughly constant pressure).
The key takeaway
If you heat air without adding moisture, W stays (almost) the same, but RH dropsbecause the saturation limit rises with temperature. If you cool air at constant W, RH increases until it reaches 100% (saturation), and then condensation can begin.
When to use each in HVAC
- Use RH for comfort, indoor air quality discussions, and “risk of saturation” intuition.
- Use W for moisture load calculations, mixing, and any process where “absolute moisture” is the right conserved quantity.
- For condensation risk on surfaces, dew point is often the most direct metric.
Related concepts
- Dew Point: condensation begins when a surface is below the air dew point.
- Specific humidity vs humidity ratio: two “absolute moisture” measures that use different denominators (moist air vs dry air).
- Wet-bulb temperature (Twb): useful for evaporative cooling and enthalpy intuition.
- Psychrometric Chart: the big picture view that contains RH, W, dew point, and more.
Using FluidTool
In the humid air tool, try this quick check: enter Tdb + RH and observe the computed W. Now change Tdb while keeping W fixed (by switching inputs to Tdb + W) and see how RH changes. This makes the difference between “relative” and “absolute” moisture very clear.