Dew Point Calculator

Enter the air temperature and relative humidity to find the dew point (Td), plus actual and saturation vapor pressure, using the Magnus-Tetens formula.

Quick Facts

Magnus-Tetens formula
Td = cγ / (b − γ)
γ = ln(RH/100) + bT/(c+T), with b = 17.625 and c = 243.04°C — accurate to about ±0.4°C for air between 0°C and 60°C.
Dew point never exceeds air temperature
Td ≤ T, always
They are equal only at 100% relative humidity, when the air is fully saturated.
Saturation vapor pressure
es = 6.1094 × e^(17.625T / (243.04+T))
In hectopascals (hPa); actual vapor pressure is e = es × RH / 100.

Your Results

Calculated
Dew Point
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Temperature at which the air becomes saturated
Actual Vapor Pressure
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e = es × RH/100, in hPa
Saturation Vapor Pressure
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es at the current air temperature, in hPa
Humidity Comfort
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Meteorological comfort scale from dew point

Ready

Enter the air temperature and relative humidity, then press Calculate.

How to Calculate Dew Point

The dew point (Td) is the temperature air would need to cool to, at constant pressure and constant moisture content, for it to become fully saturated with water vapor (100% relative humidity). Cool the air any further and excess vapor condenses into liquid water — dew on grass, fog, or condensation on a cold glass. This calculator finds dew point from air temperature and relative humidity using the Magnus-Tetens approximation of the Clausius-Clapeyron relation, the standard method used in meteorology and HVAC engineering.

How the calculation works

First the calculator finds the saturation vapor pressure at the current air temperature: es = 6.1094 × exp(17.625T / (243.04 + T)), where T is in °C and es is in hectopascals (hPa). Multiplying by relative humidity gives the actual vapor pressure already in the air: e = es × RH / 100. Inverting the Magnus formula for that actual vapor pressure yields the dew point: γ = ln(RH/100) + 17.625T / (243.04 + T), then Td = 243.04γ / (17.625 − γ). If you entered temperature in Fahrenheit, the tool converts to Celsius for the calculation and converts the result back.

Common mistakes

  • Confusing dew point with relative humidity: 50% RH at 35°C (95°F) is much more humid in absolute terms than 50% RH at 10°C (50°F) — dew point captures actual moisture content, RH does not.
  • Expecting a dew point above the air temperature: physically impossible — the maximum dew point can reach is the current air temperature, at exactly 100% RH.
  • Entering RH as a decimal instead of a percentage: use 50 for 50% humidity, not 0.5 — the formula expects RH on a 0-100 scale.
  • Using the formula far outside its tested range: the Magnus-Tetens constants used here (b = 17.625, c = 243.04) are validated for air temperatures roughly between -45°C and 60°C; extreme cold uses a separate ice-based formula.

Real-world applications

  • Meteorologists use dew point rather than relative humidity to describe how muggy the air will feel, since it does not change just because the temperature does.
  • HVAC and building engineers use dew point to size dehumidifiers and to predict condensation risk on cold surfaces like windows, ductwork, or pipes.
  • Agriculture and viticulture use overnight dew point forecasts to anticipate frost, dew formation, and fungal disease risk on crops.
  • Aviation uses the spread between air temperature and dew point to estimate cloud base height and fog formation risk.

Frequently Asked Questions

What is dew point, and how is it different from relative humidity?
Dew point is the temperature air would need to cool to (at constant pressure and moisture content) to become fully saturated, causing water vapor to condense. Unlike relative humidity, which changes with temperature even if the actual moisture in the air stays the same, dew point is a direct measure of how much water vapor is in the air — a higher dew point always means more moisture.
What formula does this calculator use?
It uses the Magnus-Tetens approximation: saturation vapor pressure es = 6.1094 × exp(17.625T / (243.04 + T)) in hPa, actual vapor pressure e = es × RH/100, and dew point Td = (243.04 × γ) / (17.625 − γ), where γ = ln(RH/100) + 17.625T/(243.04 + T). This form is accurate to about ±0.4°C for temperatures between 0°C and 60°C.
Why can the dew point never be higher than the air temperature?
The dew point is the temperature at which the current amount of water vapor would saturate the air (100% relative humidity). Since relative humidity cannot exceed 100% at the current air temperature, the dew point can only equal the air temperature (at saturation) or be lower — never higher.
What dew point feels comfortable versus muggy?
Meteorologists generally consider a dew point below 55°F (13°C) dry and comfortable, 55-65°F (13-18°C) noticeably humid, and above 65°F (18°C) muggy to oppressive. Relative humidity alone can be misleading for comfort because it depends on temperature, while dew point tracks the actual moisture content of the air.