🌡️ Known Inputs
°F

Standard thermometer reading. Measured in shade, away from moisture.

°F

Thermometer with wet wick. Always ≤ dry bulb temperature.

ft

0 ft = sea level. Denver ≈ 5,280 ft. Affects atmospheric pressure.

— % RH
Relative Humidity (live estimate)
—°
Dew Point
— gr/lb
Humidity Ratio
— BTU/lb
Enthalpy

Calculating psychrometric properties…


Psychrometrics — What It Is and Why HVAC Engineers Need It

Psychrometrics is the science of moist air. It describes all the thermodynamic properties of air-water vapor mixtures. Understanding it is fundamental to HVAC system design, load calculations, and indoor air quality.

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Dry Bulb vs Wet Bulb Temperature

The dry bulb is what a regular thermometer reads — just air temperature. The wet bulb is measured with a thermometer wrapped in a wet wick. As water evaporates, it cools the bulb. The difference between the two tells you how much moisture is in the air. A big difference means dry air; a small difference means humid air.

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Dew Point Temperature

The dew point is the temperature at which air must be cooled before water vapor starts to condense. It’s a direct measure of absolute moisture content. If you know the dew point, you know how much water is actually in the air — regardless of the dry bulb temperature. Higher dew point = more moisture = more cooling work for your AC.

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Relative Humidity vs Absolute Humidity

Relative humidity (RH) is the percentage of maximum possible moisture at a given temperature. It changes as temperature changes — even with no change in moisture content. Absolute humidity (humidity ratio W) stays constant until you actually add or remove moisture. HVAC systems must control both to keep occupants comfortable.

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Enthalpy — Total Heat Content

Enthalpy is the total energy of moist air — both the heat in the dry air (sensible heat) and the heat hidden in the water vapor (latent heat). HVAC equipment removes or adds both types of heat. Knowing the enthalpy difference between supply and return air, combined with airflow, tells you the exact cooling or heating capacity of your system.

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Specific Volume

Specific volume is the volume of moist air per unit mass of dry air (ft³/lb or m³/kg). It increases with temperature and altitude. This matters in fan and duct design — because fans move volume (CFM), not mass, but your load calculations are in mass units. At high altitude, air is less dense, so you need more CFM to deliver the same mass flow and cooling capacity.

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The Psychrometric Chart

The psychrometric chart is a visual map of all possible air states. Every point on the chart represents one specific combination of air properties. HVAC engineers plot supply, return, and mixed air conditions on this chart to visualize cooling, heating, dehumidification, and humidification processes — and to check that system performance matches design targets.

📐 Key Psychrometric Formulas

Saturation Pressure: Pws = exp(A − B/T)  [Tetens formula, T in Kelvin] Humidity Ratio: W = 0.62198 × Pw / (P − Pw)  [lbs water / lb dry air] Relative Humidity: φ = Pw / Pws × 100% Enthalpy: h = 0.240×T + W×(1061 + 0.444×T)  [BTU/lb dry air, T in °F] Specific Volume: v = 0.3704 × (T + 459.67) / (P − Pw)  [ft³/lb dry air] Wet Bulb (approx): Twb ≈ Tdb − (Tdb − Tdp) / (Cp_air / (Cp_air + W × hfg))

Where: T = temperature (°F), Pw = partial pressure of water vapor (psia), P = atmospheric pressure (psia), Pws = saturation pressure of water vapor (psia). For SI units, substitute temperature in °C and pressure in kPa. These equations are numerically iterated in this calculator for accurate results at all temperatures, humidities, and elevations.


Air Properties at Common Conditions

Reference values at sea level (14.696 psia). Useful for quick sanity-checks.

ConditionDB (°F)RH (%)Dew Point (°F)Enthalpy (BTU/lb)W (gr/lb)
Cold dry winter4030%8°F10.614.5
ASHRAE winter comfort7040%45°F26.543.4
ASHRAE summer comfort7550%55°F28.165.9
Hot humid summer9070%78°F42.2129.6
Outdoor Miami summer9175%81°F45.4141.1
Typical AC supply air5590%52°F22.978.6
Very hot dry desert11015%61°F43.788.9
Fog / saturation60100%60°F26.477.2

Frequently Asked Questions

The dry bulb temperature is what a regular thermometer reads — the standard air temperature. The wet bulb temperature is measured using a thermometer with a wet cotton wick around the bulb. As water evaporates from the wick, it cools the bulb below the air temperature. In completely dry air, evaporation is maximum and wet bulb is far below dry bulb. In fully saturated air (100% RH), there’s no evaporation and wet bulb equals dry bulb. The difference between them (called the wet bulb depression) directly indicates relative humidity.
The Magnus formula gives a good approximation: Td = (243.04 × [ln(RH/100) + (17.625×T)/(243.04+T)]) ÷ (17.625 − [ln(RH/100) + (17.625×T)/(243.04+T)]). Where T is dry bulb in °C and RH is relative humidity in %. This calculator uses a more accurate iterative method based on ASHRAE fundamentals. For a quick rule of thumb: the dew point drops about 1°C for every 5% decrease in relative humidity (when RH is above 50%).
Enthalpy is the total energy content of moist air — it includes both sensible heat (temperature) and latent heat (moisture). In Imperial units, it’s measured in BTU per pound of dry air. Enthalpy matters in HVAC because it lets you calculate the total cooling or heating capacity of your equipment. The formula is simple: Total Load (BTU/hr) = 4.5 × CFM × ΔEnthalpy (BTU/lb). Where 4.5 is a conversion factor (density × 60 minutes). This is why enthalpy is shown on every psychrometric chart.
ASHRAE Standard 55 defines the acceptable range for most occupied spaces as 30–60% relative humidity. Below 30%, occupants feel dry — static electricity, dry skin, and irritated respiratory passages become issues. Above 60%, condensation risk increases and mold growth becomes possible. The “sweet spot” for most office and residential applications is 40–55% RH. Healthcare facilities and server rooms have more specific requirements due to hygroscopic equipment and sterility needs.
At higher altitude, atmospheric pressure is lower. This affects two things: (1) The specific volume of air increases — air is less dense — so the same CFM of airflow carries less mass and less cooling capacity. A fan moves the same volume but less mass. (2) The moisture-holding capacity of air changes slightly. For Denver (5,280 ft), atmospheric pressure is about 12.2 psia vs 14.7 psia at sea level. HVAC equipment sized for sea level may underperform at altitude by 10–20%. This calculator adjusts all calculations for your specified elevation.
The Sensible Heat Ratio is the fraction of total cooling load that is sensible (temperature-related) vs latent (moisture-related). SHR = Sensible Load ÷ Total Load. A typical office space might have an SHR of 0.7–0.8, meaning 70–80% of the cooling load is sensible. Humid climates have lower SHR (more latent load). HVAC equipment must be selected to match the SHR — a unit with high SHR (designed for dry climates) in a humid climate will cool the space but fail to adequately dehumidify.
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