Thermodynamics

Psychrometric Calculator Calculator

Moist-air properties — humidity ratio, relative humidity, wet-bulb, dew point, enthalpy, and specific volume — from dry-bulb temperature and one humidity input.

W = 0.621945·Pw/(P − Pw); h = 1.006·T + W·(2501 + 1.86·T)

How it works

From the dry-bulb temperature and one humidity measure (relative humidity, wet-bulb, or dew point), the tool finds the water-vapour partial pressure, then the humidity ratio and every other moist-air property using the ASHRAE ideal-gas psychrometric relations.

Worked example

Air at 25 °C dry-bulb and 50 % relative humidity at sea level. ≈ 9.9 g of water per kg of dry air, a 17.9 °C wet-bulb, a 13.9 °C dew point, and about 50.4 kJ/kg of enthalpy.

Inputs

Frequently asked questions

What is the humidity ratio?

The mass of water vapour per unit mass of dry air (kg/kg or g/kg). Unlike relative humidity it doesn't change when you heat or cool the air without adding or removing moisture, which makes it the natural variable for HVAC and drying calculations.

What is the difference between wet-bulb and dew point?

The dew point is the temperature at which the air becomes saturated on cooling (condensation starts); the wet-bulb is the temperature reached by evaporative cooling. They are equal only at saturation — otherwise the wet-bulb sits between the dew point and the dry-bulb.

Why does pressure (altitude) matter?

Humidity ratio and specific volume depend on the total pressure, which falls with altitude — about 89.9 kPa at 1000 m versus 101.3 kPa at sea level. Using sea-level pressure at altitude introduces a real error.

Assumptions

References

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