Updated October 2026
"Absolute humidity" is one of the most misused terms in everyday humidity discussion — people often use it loosely to mean what this calculator actually reports as humidity ratio, when it technically refers to something else entirely. Here's the precise distinction, with real numbers.
Absolute humidity is derived from vapor pressure using the ideal gas law applied to the water vapor component alone: absolute humidity = e / (Rv × T), where Rv = 461.5 J/(kg·K) is the specific gas constant for water vapor and T is absolute temperature in kelvin. At 25°C, 50% RH (e = 1.584 kPa = 1,584 Pa, T = 298.15 K): absolute humidity = 1,584 / (461.5 × 298.15) ≈ 0.01151 kg/m³ = 11.5 g/m³.
Compare that to this calculator's humidity ratio for the same air: 9.88 g per kg of dry air. The two numbers are close in this particular case but represent genuinely different physical quantities — one is water vapor mass per volume of moist air, the other is water vapor mass per mass of dry air — and they diverge more at different temperatures and pressures because humidity ratio doesn't depend on air density at all, while absolute humidity does.
Humidity ratio (mass per mass of dry air) stays constant through simple heating or cooling with no moisture added or removed — which is exactly the property HVAC load calculations, dehumidifier sizing and duct/coil moisture balances need. Absolute humidity (mass per volume) changes with temperature and pressure alone, even with zero moisture actually added or removed, simply because volume expands or contracts — making it a less convenient basis for engineering calculations, even though it's a perfectly valid physical quantity in its own right.