Relative humidity (RH) is the Percentage ratio between the pressure of water vapor in the air and the pressure of saturated vapor at a given temperature.
In other words, it is the Humidity level present in the air compared to the maximum quantity that the air can contain before condensation.
This measure varies according to the Room temperature : the hotter the air, the more water vapor it can contain without reaching the saturation point. That's why we talk about rates relative : at 20°C, 50% relative humidity does not represent the same quantity of water as 50% at 30°C.
🌡️ Example: at 25°C, a 60% relative humidity level means that the air contains 60% of the water vapor that it could potentially retain before saturation.
It's the most used value in the areas of building, of the logistics, or even Indoor humidity control, because it provides simple and directly usable information. In particular, it makes it possible to:
Absolute humidity (HA) corresponds to the Mass of water vapor contained in a given volume of air, expressed in g/m³. Contrary to relative humidity, It does not depend on the temperature.
For example, 10 g/m³ means that every cubic meter of air contains 10 grams of water vapor, regardless of thermal conditions.
Absolute humidity is less commonly used on a daily basis, but very useful for:
The two are complementary for a good humidity control in a space.