+**Relative Humidity** is a measure of the amount of water vapor in the air relative to the maximum amount the air can hold at a specific [Temperature](/wiki/temperature). Expressed as a percentage, it indicates how "saturated" the air is with moisture, playing a crucial role in [Weather](/wiki/weather) and human comfort. When relative humidity reaches 100%, the air is saturated, often leading to condensation or precipitation.
+## See also
+- [Absolute Humidity](/wiki/absolute_humidity)
+- [Dew Point](/wiki/dew_point)
+- [Evaporation](/wiki/evaporation)
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