A wet thermometer explains the idea

Wrap a thermometer sensor in a wet cloth and ventilate it. Water evaporates, using heat taken from the sensor, which cools down. The temperature it reaches is the wet-bulb temperature, expressed in degrees Celsius.

Dry air and damp air behave differently

  • Dry air: Water evaporates readily. The wet thermometer reads well below a dry one.
  • Humid air: Evaporation provides less cooling. The two readings are closer.
  • Saturated air: Wet-bulb temperature, dew point and air temperature coincide under ordinary conditions.

What the value is useful for

The same principle explains cooling by evaporating sweat. A high wet-bulb temperature indicates limited cooling from evaporation. Actual heat strain also depends on sunshine, wind, activity and clothing.

The value is useful for snowfall too: evaporation and melting can cool air during precipitation. Wet-bulb temperature is not the heat index, nor is it WBGT, which includes further weather effects. A single number cannot supply a safety threshold that applies to everyone.

Back to Weather Glossary

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