By Robin McDaniel | Updated Aug 30, 2022
Accurately gauging the moisture content of the air—known as relative humidity (RH)—is essential for weather‑related projects, scientific experiments, and everyday comfort. This guide walks you through a reliable method using basic equipment and straightforward calculations.
Acquire two bulb thermometers with round, cylindrical bulbs and Fahrenheit scales. Place them on a stable surface where they can freely stand and remain exposed to ambient air.
The dry‑bulb reading represents the actual air temperature. Because humidity increases with temperature, this measurement is critical. Set the thermometer in a neutral, dry spot away from direct sunlight to capture an accurate air temperature.
Wrap the bulb of a second thermometer in a wet muslin cloth and allow air to flow over it normally. As the moisture evaporates, the wet‑bulb temperature drops, revealing the air’s moisture level.
Use a psychrometric chart, slide rule, or calculator to plot the dry‑ and wet‑bulb temperatures. The intersection of their lines gives the dew point, a key value for computing RH.
First, convert Fahrenheit to Celsius:
ÅC = (5/9) × (ÅF – 32). For the dew point, apply the same formula to the wet‑bulb reading.
Next, compute the actual vapor pressure (Ea) and saturated vapor pressure (Es):
Ea = 6.11 × 107.5 Tc/(237.7 + Tc)
Es = 6.11 × 107.5 Td/(237.7 + Td) (Tc = Celsius air temp, Td = Celsius dew point).
Relative Humidity (%) = (Ea ÷ Es) × 100. The result is the air’s moisture content expressed as a percentage.
Results may differ by 10% or more due to environmental variations and instrument accuracy. Use the procedure as a reliable estimate rather than an absolute measurement.