🔬
🔬 Science & engineering

Absolute Humidity Calculator (g/m³ of water vapor from temperature and RH)

Results update as you type.

Your numbers

Understanding the absolute humidity calculator — concept and principle

Absolute humidity is the mass of water vapour in one cubic metre of air. This calculator finds it from air temperature and relative humidity, and also gives the vapour pressure, humidity ratio, specific humidity and dew point. It is useful in HVAC, drying, storage, meteorology and indoor-climate work.

Water vapour in 1 m³ of air at 25 °CWater vapour in 1 m³ of air at 25 °CWater vapour in 1 m³ of air at 25 °Cat 60% RH13.82 gat saturation23.03 gDew point 16.7 °C · vapour pressure 19.02 hPa
At 25 °C and 60% RH each cubic metre holds 13.82 g of water vapour; surfaces below 16.7 °C would collect dew.

How it is calculated

The principle

Warm air can hold more water vapour than cold air, so relative humidity alone does not tell you how much water is present. Absolute humidity does. Treating water vapour as an ideal gas, its density follows from its partial pressure and temperature. The humidity ratio, used in psychrometrics, compares the mass of vapour with the mass of dry air, which is why it depends on the total air pressure.

Worked example

Default inputs: 25 °C, relative humidity 60%, pressure 101.325 kPa.

  1. Saturation vapour pressure at 25 °C ≈ 31.69 hPa.
  2. Vapour pressure = 0.60 × 31.69 ≈ 19.02 hPa.
  3. AH = 1,902 Pa ÷ (461.5 × 298.15 K) ≈ 0.01382 kg/m³ = 13.82 g/m³; at saturation 23.03 g/m³.
  4. Humidity ratio = 0.621945 × 1.902 ÷ (101.325 − 1.902) ≈ 11.9 g/kg dry air; specific humidity ≈ 11.76 g/kg.
  5. Dew point ≈ 16.7 °C.
How Absolute humidity (g/m³) changes with Air temperature (°C)How Absolute humidity changes with Air t…010203040506.2512.518.82531.237.550Example: 13.82Air temperature (°C)
Each point is the calculator re-run with only “Air temperature (°C)” changed; the gold point is the default example. Change the inputs above and this chart follows your numbers.
Air temperature (°C)Absolute humidity (g/m³)
6.254.43
12.56.6
18.89.64
2513.82
31.219.48
37.527.01
5049.68

How to read the result

The dew point is often the most practical number: surfaces colder than 16.7 °C in this air will gather condensation. Absolute humidity lets you compare air at different temperatures; for example, cold outdoor air at high RH may contain far less water than warm indoor air at moderate RH.

Common mistakes

Keep in mind: Results assume ideal-gas behaviour and accurate sensor readings. For HVAC design or building moisture control, use local codes and consult a qualified professional.

Frequently asked questions

What is the difference between absolute and relative humidity?

Absolute humidity is the actual mass of water vapour per volume; relative humidity is the vapour pressure as a percentage of the saturation value at that temperature.

What is a comfortable indoor humidity?

Comfort and health guidance often cites relative humidity of roughly 30–60% indoors; check guidance relevant to your setting.

How is dew point related to absolute humidity?

Both depend only on the amount of water vapour; the dew point is the temperature at which that vapour would saturate the air.

Sources: ASHRAE Handbook — Fundamentals, Chapter 1 Psychrometrics · WMO, Guide to Instruments and Methods of Observation (WMO-No. 8), humidity

Checked 9 Nov 2026. ASHRAE Handbook — Fundamentals (2017), ch. 1 “Psychrometrics”, eqs. 5–6 (saturation pressure), 20, 26, 30, 33 and 35, as implemented in PsychroLib (Meyer & Thévenard, J. Open Source Software 4(33):1137, 2019; R source psychrolib.R); water-vapor gas constant R/Mw = 8.314462618 ÷ 0.01801528 = 461.52 J/(kg·K) (standard values).

🔬 All science & engineering tools →🌍 Calculators by country →