- Air temperature
- 25°C
- Relative humidity
- 60%
13.815g/m³
Open with these values13.815g/m³
Result: 13.815 g/m³Relative humidity alone says nothing about how much water the air holds: 80 % at 30 °C carries almost three times the water of 80 % at 10 °C. Enter temperature and relative humidity and read the vapour in grams per cubic metre — the number behind drying, storage and condensation.
Held fixed: Air temperature 25.0 °C.
| Relative humidity (%) | Result (g/m³) |
|---|---|
| 40.0 | 9.210 |
| 50.0 | 11.513 |
| 60.0Your value | 13.815 |
| 70.0 | 16.118 |
| 80.0 | 18.420 |
13.815g/m³
Open with these values8.454g/m³
Open with these values15.843g/m³
Open with these valuesAH = 2.1674 × 6.112 × e^(17.67·T ÷ (T + 243.5)) × RH ÷ (273.15 + T)
| Temperature, humidity | Air | Water vapour |
|---|---|---|
| -10, 80 | Winter frost | 1.890 |
| 0, 100 | Freezing fog | 4.850 |
| 10, 90 | Cool and damp | 8.454 |
| 20, 50 | Living room | 8.639 |
| 25, 60 | Warm summer day | 13.815 |
| 30, 80 | Tropical | 24.283 |
| 35, 40 | Hot and dry | 15.843 |
The mass of water vapour in one cubic metre of air, given in grams. Unlike relative humidity it does not change when the air is heated or cooled, as long as no water is added or removed.
Because relative humidity is measured against what the air could hold at that temperature, and cold air can hold very little. The table shows both cases at roughly 8.5 grams per cubic metre.
Only slightly, and this formula ignores it. Water vapour follows its own partial pressure, so the result holds at sea level and on a mountain alike.
The Magnus approximation behind the saturation pressure is good to about 0.3 % between -40 °C and 50 °C. That is far finer than a household hygrometer, which typically reads within 3 % of relative humidity.
Multiply the result by the room volume in cubic metres. A room of 50 cubic metres at 25 °C and 60 % relative humidity holds about 690 grams of water vapour.
Information, not professional advice.
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