Psychrometric Calculator
Calculate all moist air properties from any two inputs using ASHRAE Hyland-Wexler equations. Altitude-corrected. Includes process calculator for heating, cooling, and dehumidification analysis.
Calculate all moist air properties from any two inputs using ASHRAE Hyland-Wexler equations. Altitude-corrected. Includes process calculator for heating, cooling, and dehumidification analysis.
A psychrometric chart maps the thermodynamic properties of moist air at a given barometric pressure. Given any two independent properties, all other properties are fixed. This calculator replaces chart reading with precise ASHRAE equations, giving you exact values instead of interpolated readings.
Dry-bulb temperature is the standard air temperature measured by a thermometer. Wet-bulb temperature is measured with a wetted wick and reflects the cooling effect of evaporation. The difference between them (wet-bulb depression) indicates how much moisture the air can absorb — critical for cooling tower sizing and evaporative cooling.
Psychrometric properties depend on barometric pressure. At higher elevations, lower air pressure changes humidity ratios, specific volumes, and enthalpy values. A 5,000 ft elevation reduces pressure by about 17%. Always use altitude-corrected values for accurate HVAC design above 2,000 ft.
The process calculator shows what happens when air moves through HVAC equipment. Enter the entering and leaving conditions to see sensible heat (temperature change), latent heat (moisture change), and total heat. The sensible heat ratio (SHR) is critical for coil selection — typical comfort cooling has an SHR of 0.7-0.8.
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