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  • How to Measure Relative Humidity: A Practical Guide for Students and Weather Enthusiasts

    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.

    Step 1 – Gather Your Instruments

    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.

    Step 2 – Measure the Dry‑Bulb Temperature

    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.

    Step 3 – Measure the Wet‑Bulb 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.

    Step 4 – Determine the Dew Point

    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.

    Step 5 – Apply the Calculations

    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).

    Step 6 – Calculate Relative Humidity

    Relative Humidity (%) = (Ea ÷ Es) × 100. The result is the air’s moisture content expressed as a percentage.

    Things Needed

    • Bulb thermometers (dry and wet)
    • Muslin cloth
    • Water (for wetting the cloth)
    • Psychrometric slide rule or digital calculator
    • Psychrometric graph or software

    Warning

    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.

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