HVAC and cooling
Estimate entering wet bulb, evaporative cooling potential, air enthalpy, moisture loading, and pressure-sensitive system behavior.
Calculate wet-bulb temperature, humidity properties, cooling potential, and pressure effects. Compare methods, analyze scenarios, export reports, and process complete weather datasets.
Select an input mode. Irrelevant fields are hidden automatically.
Load common environments, then adjust any input.
Process up to 500 rows in Celsius, percent, kilopascals, and metres.
Recent results are stored only in the current PHP session.
No calculations are stored yet.
The default workflow derives vapor pressure, humidity ratio, enthalpy, and saturated wet-bulb state.
The calculator first determines actual vapor pressure from the selected input pair. It then calculates humidity ratio at the specified atmospheric pressure.
The solver finds a saturated temperature whose moist-air enthalpy matches the initial state.
This method relates measured dry-bulb and wet-bulb readings to vapor pressure. The coefficient changes with the selected instrument type.
This empirical equation provides a fast sea-level estimate from Celsius temperature and relative humidity.
Real coolers approach wet-bulb temperature according to their saturation efficiency.
Estimate entering wet bulb, evaporative cooling potential, air enthalpy, moisture loading, and pressure-sensitive system behavior.
Review greenhouse cooling potential, livestock housing conditions, fogging suitability, crop environment, and grain-drying context.
Compare hot-dry, hot-humid, high-altitude, near-saturation, and cold-weather atmospheric states.
Explore relationships among dry bulb, wet bulb, dew point, relative humidity, pressure, enthalpy, and humidity ratio.
Screen evaporative drying, ventilation, air treatment, storage, process-air, and environmental control conditions.
Use wet bulb as one environmental clue while following approved WBGT, workplace, athletic, and public-health protocols.
It is the equilibrium temperature approached by a wetted, ventilated sensor as water evaporates into the surrounding air.
Evaporation consumes energy and cools the wetted surface. The temperatures become equal when the air is saturated.
No. Dew point describes saturation by cooling at nearly constant moisture content. Wet bulb includes evaporative cooling and energy exchange.
No. WBGT is a separate heat-stress index that may include natural wet bulb, globe temperature, and dry-bulb temperature.
Humidity ratio and evaporation relationships depend on total atmospheric pressure. Elevation can therefore change detailed psychrometric results.
Use the pressure-corrected iterative method for general analysis. Use Stull for a fast estimate within its published range.
No. Input sensor quality, airflow, radiation shielding, wick condition, and water purity affect physical measurements.
It describes how closely an evaporative cooler approaches the theoretical wet-bulb temperature under its operating conditions.
Use temperature in Celsius, relative humidity percent, optional pressure in kilopascals, and optional elevation in metres.
They represent different approximations and definitions. Empirical, psychrometer, and thermodynamic methods can differ slightly.
Yes. Select target-condition mode, enter dry bulb and target wet bulb, then solve for required relative humidity.
The same file exposes a simple read-only JSON endpoint for internal integrations.
?api=1&dry_bulb=30&relative_humidity=50&pressure=101.325&temperature_unit=cRate limiting should be added at the web-server or reverse-proxy layer for public deployments.
Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.