Absolute humidity (\(d_v\)) is the total mass of water vapor (\(m_{H_2O}\)) present in a given volume of air (\(V_{air}\)). It is expressed as grams of water vapor per cubic meter of air (\(g/m^3\)). The formula is \(d_v = \frac{m_{H_2O}}{V_{air}}\). Unlike relative humidity, it is not dependent on the air’s temperature, but it is affected by changes in air pressure or volume.





