Linked from

The 16 pages that link to Wet-bulb temperature, each with the reason it gives.

• Evaporative coolingRelated: It sets a practical limit for direct evaporative cooling.

• Relative humidityRelated: It connects humidity to evaporative cooling and human heat limits.

• Heat waveRelated: It helps assess whether sweat can cool the body effectively in hot, humid conditions.

• Dew pointCompared with: It is generally above dew point and measures evaporative cooling rather than saturation by cooling.

• HumidityRelated: Its difference from dry-bulb temperature helps determine humidity in psychrometric measurements.

• ThunderstormRelated: Evaporative cooling in rain shafts can contribute to strong thunderstorm downdrafts.

• Cooling towerRelated: It sets a practical lower limit for cooling tower water temperature.

• Heat stressRelated: Its limits are studied as indicators of when human heat loss becomes difficult.

• PsychrometricsRelated: Evaporative cooling links this measurement to air moisture and enthalpy.

• Freezing rainRelated: It helps forecasters assess whether near-surface air can cool enough to support freezing precipitation.

• Lifting condensation levelCompared with: It is an evaporation-based temperature, unlike the parcel’s dew-point temperature at saturation.

• VirgaRelated: Evaporation cools the air and precipitation toward this temperature.

• Evaporative coolerRelated: It sets the practical lower limit for direct evaporative cooling.

• Climate change in the Middle East and North AfricaRelated: Rising heat and humidity can push outdoor conditions toward dangerous limits.

• Ice pelletsRelated: It helps determine whether falling snow melts in a warm layer.

• Rain and snow mixedRelated: It helps determine whether falling snow melts near the surface.