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Vapor Pressure of Water Calculator — 0–100°C | LazyTools
Math & Science

Vapor Pressure of Water Calculator

Calculate the saturation vapour pressure of water at any temperature from 0 to 100°C using the NIST Antoine equation. Furthermore, results are shown in mmHg, kPa, atm, and bar alongside the absolute humidity (saturation water content in g/m³) — essential for HVAC, meteorology, and chemistry.

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Valid range: 0°C to 100°C. Uses Antoine equation with NIST constants. Above 100°C see steam tables.

How to use the Vapor Pressure of Water Calculator

1
Enter temperature

Type the temperature in °C, K, or °F. Furthermore, valid range is 0–100°C (32–212°F, 273–373 K). Above 100°C, consult steam tables.

2
Click Calculate

Vapour pressure appears in four units plus absolute humidity at saturation. Moreover, absolute humidity at saturation = P°×M_w/(R×T) in g/m³.

3
Read absolute humidity

Absolute humidity at saturation is the maximum water vapour content of air at that temperature. Furthermore, actual humidity = RH% × saturation humidity.

4
Apply to dew point calculations

Dew point is the temperature at which current water vapour pressure equals the saturation vapour pressure. Furthermore, at 50% RH and 25°C: P_actual = 0.5 × 23.8 = 11.9 mmHg → dew point ≈ 13.8°C.

5
Use in Raoult's law and Henry's law

P° (water) at the process temperature feeds into Raoult's law for aqueous mixture vapour pressures and Henry's law for gas solubility. Moreover, cooling towers and evaporative coolers use water vapour pressure extensively.

Variants, options and when to use each

TemperatureP° (mmHg)P° (kPa)Abs. humidity (g/m³)
0°C4.580.6114.85
10°C9.211.2289.40
20°C17.52.33817.3
25°C23.83.16723.0
37°C46.66.21144.0
100°C760101.3597

The formula explained

log₁₀(P) = 8.07131 − 1730.63/(233.426 + T°C) | AH = P° × M_w / (R × T)
= saturation vapour pressure (mmHg)
T°C = temperature in Celsius
AH = absolute humidity at saturation (g/m³)
M_w = 18.015 g/mol (molar mass of water)
R = 8.314 J/mol·K

The Antoine equation with NIST constants A=8.07131, B=1730.63, C=233.426 gives log₁₀(P/mmHg) as a function of temperature. Furthermore, the constants are valid over 1–100°C and reproduce the NIST steam tables to within 0.1%. Moreover, absolute humidity AH = P°×M_w/(R×T) derives from the ideal gas law — treating water vapour as an ideal gas.

Worked example — dew point from relative humidity

Air at 25°C, RH = 60%. Find the dew point. Furthermore, P°(25°C) = 23.8 mmHg.

StepCalculationResult
Partial pressure of water0.60 × 23.814.28 mmHg
Dew point: find T where P° = 14.28Inverse AntoineTdp ≈ 16.5°C
Condensation risk?Surface below 16.5°CCondensation will form
At 25°C and 60% RH, the dew point is ~16.5°C. Furthermore, any surface colder than 16.5°C will show condensation — important for insulation design, electronics cooling, and food storage. Moreover, human comfort zone is approximately 10–20°C dew point — above 20°C dew point feels oppressively humid; below 5°C feels very dry.

What is the saturation vapour pressure of water?

The saturation vapour pressure of water P° is the partial pressure of water vapour in thermodynamic equilibrium with liquid water at a given temperature. Furthermore, it increases rapidly with temperature — roughly doubling every 10°C near room temperature. At 100°C, P° = 760 mmHg = 1 atm, which is the definition of the normal boiling point.

Relative humidity RH = (actual water vapour pressure / P°) × 100%. Moreover, when RH = 100%, the air is saturated — no more water can evaporate, and any cooling causes condensation (fog, dew, or frost). The dew point is the temperature at which the actual water vapour pressure equals P° — cooling below this temperature causes condensation.

Absolute humidity (g/m³) measures the actual mass of water vapour per unit volume of air. Additionally, it is directly proportional to water vapour pressure through the ideal gas law: AH = P × M_w/(RT). At saturation, AH = P° × M_w/(RT) — this is the maximum water vapour content of air at temperature T.

Who uses this calculator?

Meteorologists calculate dew point, relative humidity, and fog formation from water vapour pressure. Furthermore, HVAC engineers size cooling coils using the saturation vapour pressure at different temperatures for dehumidification calculations. Food scientists control water activity in dried foods using water vapour pressure relationships. Moreover, industrial drying engineers (freeze dryers, spray dryers, tunnel dryers) use P° to calculate evaporation driving force and outlet air humidity.

Historical context and related concepts

The relationship between temperature and vapour pressure of water was measured by Dalton (1801) and systematically tabulated throughout the 19th century. Furthermore, the thermodynamic basis was provided by Clausius and Clapeyron (1834–1850). NIST has maintained steam tables since the 1930s — the current IAPWS-IF97 formulation covers 0–800°C to extremely high precision. Moreover, the Antoine equation remains the standard simple formula for educational and routine engineering calculations.

Why water vapour pressure calculations underpin HVAC, meteorology, and food safety

Air conditioning systems must remove sufficient water vapour from air to maintain comfortable humidity levels. Furthermore, the cooling coil must be below the dew point of the incoming air — the amount of condensate removed determines the dehumidification capacity. A 1°C error in dew point calculation corresponds to significant moisture load errors in large commercial HVAC systems. Moreover, food water activity (aw = P/P°) directly controls microbial growth — products above aw = 0.85 support most bacteria.

Water vapour pressure in climate science and global warming

Water vapour is the most abundant greenhouse gas — responsible for about 50% of the greenhouse effect. Furthermore, as CO₂ warms the atmosphere, higher temperatures allow more water vapour (following the Antoine equation), amplifying warming — the water vapour feedback. A 1°C temperature increase increases P° by ~7%, allowing ~7% more atmospheric water vapour. Moreover, this positive feedback roughly doubles the warming from CO₂ alone — the key amplification mechanism in climate models.

Frequently asked questions

Vapour pressure P° is the maximum partial pressure of water vapour in equilibrium with liquid water at a given temperature. Partial pressure is the actual pressure of water vapour in a gas mixture, which may be less than P° (unsaturated air, RH < 100%). Furthermore, P_actual = RH/100 × P°. When P_actual = P°, RH = 100% and the air is saturated. Moreover, above P°, excess vapour would spontaneously condense.
1 atm = 760 mmHg = 101.325 kPa = 1.01325 bar = 14.696 psi. Furthermore, to convert mmHg to kPa: multiply by 0.133322. To convert kPa to mmHg: multiply by 7.50062. Moreover, in the SI system, kPa is standard for vapour pressures; mmHg is still widely used in clinical and atmospheric contexts.
Water activity aw = P/P° — the ratio of the partial pressure of water above a food sample to the pure water vapour pressure at the same temperature. Furthermore, aw = 1 for pure liquid water; aw < 1 for any mixture or solid containing water. Most bacteria require aw > 0.91; fungi can grow at aw > 0.80. Moreover, measuring aw uses a humidity sensor at equilibrium with the sample — reading aw = RH/100 at equilibrium.
At 25°C: water P° = 23.8 mmHg; ethylene glycol = 0.06 mmHg; glycerol = 0.0001 mmHg. Furthermore, water has extensive hydrogen bonding but a very small molecule — at 25°C, thermal energy is sufficient to overcome the intermolecular forces for significant evaporation. Glycerol and ethylene glycol have much larger molecules and more hydrogen bonds — much lower P°. Moreover, this is why water evaporates readily from skin but glycerol-based hand creams do not.
Dew point Td is the temperature at which P° (Td) = P_actual = (RH/100) × P° (T_air). Furthermore, given T and RH: P_actual = (RH/100) × P°(T). Then solve Antoine equation for T where P° = P_actual. Moreover, the Magnus formula approximates dew point: Td ≈ T − (100−RH)/5 (°C) — valid within a few °C for typical conditions.

Related tools

Vapor Pressure Calculator

Antoine equation for 6 solvents including water. Furthermore, this calculator is the water-specific version.

Raoult's Law Calculator

Mixture vapour pressure. Moreover, water P° from Antoine feeds into Raoult's law for aqueous solutions.

Henry's Law Calculator

Dissolved gas at equilibrium. Furthermore, water vapour pressure determines atmospheric water absorption.

Boiling Point Elevation Calculator

Solutes raise boiling point by reducing water vapour pressure. Moreover, boiling point elevation = vapour pressure depression effect.

Significant Figures Calculator

Round vapour pressure to appropriate precision. Furthermore, Antoine equation gives 4 significant figures.

Combined Gas Law Calculator

Gas laws apply to water vapour. Moreover, water vapour partial pressure follows ideal gas law at ambient conditions.

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