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Psychrometric Calculator — Air Properties from Any Two Known Values

Calculate Dry-Bulb, Wet-Bulb, Dew Point, Relative Humidity, Enthalpy & Specific Volume

Free psychrometric property calculator for HVAC engineers, technicians, and building scientists. Enter any two known air properties and the calculator solves for all remaining psychrometric values including dry-bulb temperature, wet-bulb temperature, dew point, relative humidity, humidity ratio, enthalpy, and specific volume. Altitude-corrected for accurate results at any elevation.

Use this tool to verify field measurements, calculate cooling coil loads, check for condensation risk, size dehumidification equipment, and understand air mixing processes. Essential for commissioning, troubleshooting, and HVAC system design at any altitude from sea level to high-elevation mountain sites.

Pro Tip: When measuring wet-bulb temperature in the field, make sure your wick is saturated with distilled water and the air velocity across the wick is at least 900 fpm. A dry or slow-moving wick reads artificially high, which skews your humidity calculations and can lead to incorrect charge adjustments on fixed-orifice systems that depend on wet-bulb input.

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Psychrometric Calculator

How It Works

  1. Enter Altitude or Barometric Pressure

    Set your site elevation or barometric pressure. Psychrometric calculations depend on atmospheric pressure. At Denver (5,280 ft), atmospheric pressure is about 12.2 psia vs 14.696 at sea level. Using sea-level defaults at altitude introduces 5-15% error in humidity ratio and enthalpy.

  2. Select Two Known Properties

    Choose any two of: dry-bulb temperature, wet-bulb temperature, dew point temperature, relative humidity, or humidity ratio. The calculator solves the psychrometric equations for all remaining properties. The most common field pair is dry-bulb and relative humidity, but dry-bulb and wet-bulb is preferred for HVAC calculations.

  3. Enter Known Values

    Type in the values for your two selected properties. Use accurate instruments: a calibrated thermometer for dry-bulb, a sling psychrometer or digital hygrometer for wet-bulb or RH. The quality of results depends entirely on the accuracy of your inputs.

  4. Review All Calculated Properties

    The calculator outputs dry-bulb, wet-bulb, dew point, relative humidity, humidity ratio (grains/lb and lb/lb), enthalpy (BTU/lb), specific volume (ft3/lb), and vapor pressure. All values are altitude-corrected for your site.

  5. Apply Results to Your HVAC Problem

    Use dew point to check for condensation on cold surfaces. Use enthalpy difference across a coil to calculate cooling load. Use humidity ratio to size dehumidification. Use specific volume to convert between mass flow and volumetric flow (CFM).

Built For

  • HVAC technicians calculating wet-bulb temperature from dry-bulb and RH for superheat charging charts
  • Building scientists assessing condensation risk on windows, walls, and cold piping by comparing surface temperature to dew point
  • Engineers calculating total cooling load (sensible + latent) using enthalpy difference across air handler coils
  • Indoor air quality specialists sizing dehumidification equipment based on humidity ratio and target RH
  • Commissioning agents verifying supply and return air conditions match design specifications during system startup
  • HVAC instructors teaching psychrometric relationships with an interactive calculation tool
  • High-altitude HVAC contractors in Denver, Salt Lake City, and mountain resort towns who need altitude-corrected air properties

Features & Capabilities

Altitude Correction

Enter elevation in feet or barometric pressure in inHg/psia. All psychrometric calculations adjust for local atmospheric pressure. Critical for installations above 3,000 feet where sea-level assumptions introduce significant errors.

Any Two Input Properties

Solve from any combination of dry-bulb, wet-bulb, dew point, relative humidity, or humidity ratio. The calculator selects the correct psychrometric equations based on your input pair and solves iteratively where needed.

Complete Property Output

Returns all psychrometric properties: Tdb, Twb, Tdp, RH, W (humidity ratio), h (enthalpy), v (specific volume), and Pw (vapor pressure). Everything you need for coil calculations, duct sizing, and IAQ analysis in one output.

Unit Toggle

Switch between IP (Fahrenheit, BTU/lb, grains/lb) and SI (Celsius, kJ/kg, g/kg) units. Input in either system and the calculator converts all outputs to your preferred unit system.

Condensation Risk Flag

Compares your dew point to common surface temperatures and flags conditions where condensation is likely. Useful for assessing cold window frames, chilled water piping, and concrete slabs in contact with humid air.

PDF Export

Export your psychrometric calculation results as a branded PDF for project documentation, commissioning reports, or training records.

Frequently Asked Questions

Any two independent psychrometric properties are sufficient. The most common pairs are dry-bulb + relative humidity (easy to measure with a digital hygrometer), dry-bulb + wet-bulb (measured with a sling psychrometer), or dry-bulb + dew point (from a chilled mirror hygrometer). Dry-bulb + humidity ratio also works if you have a precise humidity sensor.
Atmospheric pressure decreases with altitude. At Denver (5,280 ft), pressure is about 83% of sea level. Since water evaporates more easily at lower pressures, the same dry-bulb and RH combination produces a different humidity ratio, enthalpy, and specific volume at altitude vs sea level. Using sea-level defaults at altitude overpredicts moisture content by 10-15%.
Dew point is the temperature at which the air becomes saturated and water condenses. Wet-bulb is the temperature measured by a thermometer with a wet wick in moving air. Both relate to moisture content, but dew point is a direct indicator of absolute moisture while wet-bulb also depends on dry-bulb temperature. In dry conditions, the wet-bulb can be well above the dew point. They converge at 100% RH where Tdb = Twb = Tdp.
Measure the air conditions entering and leaving the coil (dry-bulb and wet-bulb on each side). Look up enthalpy for both states. Total cooling load in BTU/hr = 4.5 x CFM x (h_entering - h_leaving). The factor 4.5 accounts for the density of standard air. This captures both sensible (temperature) and latent (moisture) cooling in one calculation.
Yes. If the dew point temperature is at or above the surface temperature of any wall, window, or pipe, condensation will form. Sustained surface moisture above 65% RH promotes mold growth. Calculate the dew point from your indoor conditions, then compare it to the coldest surface in the room. If the surface temperature is within a few degrees of the dew point, you have condensation risk and should improve ventilation or dehumidify.

Learn More

HVAC

Complete Guide to Superheat and Subcooling Measurements

How to measure, interpret, and diagnose refrigerant charge using superheat and subcooling. Covers TXV vs fixed-orifice charging methods, target superheat charts, common diagnostic scenarios, and measurement mistakes.

HVAC

Understanding the Psychrometric Chart for HVAC

How to read a psychrometric chart, calculate cooling coil loads from enthalpy, assess condensation risk from dew point, size dehumidification, and verify commissioning measurements. Includes altitude effects.

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