Dew Point Calculator
Calculate the dew point temperature from air temperature and relative humidity. Includes comfort level assessment and frost risk.
About this calculator
Dew Point is calculated with the Magnus formula, a standard meteorological approximation that converts Air Temperature and Relative Humidity into the temperature at which the air would become saturated and water vapor would begin condensing. Both Air Temperature and Relative Humidity push Dew Point in the same direction — warmer air or higher humidity both raise the calculated dew point — and which one moves the result more depends on where you're starting from: Air Temperature's effect grows stronger the warmer the air already is, while Relative Humidity's effect stays comparatively steady across its range, so neither input reliably dominates the other over this calculator's full declared ranges. The Magnus coefficients used here (a = 17.27, b = 237.7) are validated for air temperatures between 0°C and 60°C; below freezing the result is still the dew point over liquid water rather than the frost point over ice, which uses a different coefficient pair, so treat sub-freezing results as approximate.
Comfort Level buckets the resulting dew point (converted to Celsius internally regardless of your selected display unit) into the standard published dew-point comfort scale: a below-freezing band where the mugginess scale simply does not apply, then seven bands from "Dry & comfortable" below 10°C up to "Severely high — heat stress risk" above 24°C (75°F); dew point, not relative humidity alone, is the figure meteorologists generally consider the more reliable indicator of how humid the air actually feels, since a given relative humidity percentage means very different things at different temperatures. Frost Risk requires more than a sub-freezing dew point: actual frost needs a surface at or below freezing, which needs the air temperature itself to fall close to the dew point, so the flag distinguishes air that is already at or below freezing, air within about 10°F of its sub-freezing dew point where overnight cooling could plausibly reach it, and the ordinary case of dry warm air with a sub-freezing dew point that poses no frost risk at all. This is a physics-based formula rather than a manufacturer-calibrated instrument reading, so it will differ slightly from a dedicated dew point sensor, and it does not account for elevation, air pressure, or local microclimate effects.
Inputs
Results
Dew Point
29.2
Figures current as of 1974. Source: Psychrometry and Psychrometric Charts (1974) — origin of the a=17.27, b=237.7°C Magnus-formula coefficient pair (accurate to ±0.4°C over 0–60°C) this calculator implements.
How to Use This Calculator
- Select your Temperature Unit (Fahrenheit or Celsius).
- Enter the Air Temperature.
- Set the Relative Humidity (%).
- Review the Dew Point temperature, Comfort Level, Temp/Dewpoint Spread, and Frost Risk indication.
How the result changes with Air Temperature
| Air Temperature | Dew Point |
|---|---|
| 20 | 10.2 |
| 30 | 19.7 |
| 54 | 42.5 |
What each input means
- Temperature Unit
- Measurement system to use.
- Air Temperature
- Air temperature in the unit selected above. The range spans -40 to 54 in both scales (-40 °F to 130 °F, -40 °C to 54 °C); note that switching the unit reinterprets the number you have already typed rather than converting it.
- Relative Humidity
- Relative humidity as a percentage.
How this is calculated
Formula
Uses the Magnus formula: Td = (b × α) / (a - α), where α = (a × T) / (b + T) + ln(RH/100). Constants: a = 17.27, b = 237.7°C.Worked example, using the default values
- Identify Input Parameters3 parametersTemperature Unit = 0, Air Temperature = 40, Relative Humidity = 65 = 3 input(s) provided
- Calculate Dew PointTd = (b x alpha) / (a - alpha), alpha = (a x T)/(b + T) + ln(RH/100)29.2 = 29.2
- Calculate Comfort LevelComfort Level = band lookup on dew point in degCCold — comfort scale does not apply = Cold — comfort scale does not apply
- Calculate Temp/Dewpoint SpreadTemp/Dewpoint Spread = round((displayTemp - displayDewPoint) * 10) / 1010.8 = 10.8
Figures and sources
- Magnus formula constants used here (a = 17.27, b = 237.7°C, valid 0–60°C) (1974) — Psychrometry and Psychrometric Charts (1974) — origin of the a=17.27, b=237.7°C Magnus-formula coefficient pair (accurate to ±0.4°C over 0–60°C) this calculator implements.
Engine last updated . Checked against 2 independently-derived tests — how we verify calculators. Built by Paul Gunder, a software engineer, not a licensed financial, medical, or legal professional.
Frequently Asked Questions
Why does raising the temperature increase the calculated Dew Point even if humidity stays the same?
The Magnus formula ties dew point to both the actual vapor pressure implied by relative humidity and the reference temperature used to compute it. At a fixed relative humidity percentage, warmer air holds more total water vapor by mass, so the saturation point (dew point) rises along with air temperature even without any change to the humidity reading itself.
Is a high Comfort Level rating the same thing as high relative humidity?
Not necessarily — Comfort Level is based on Dew Point, not Relative Humidity directly, and the same relative humidity percentage produces very different dew points at different temperatures. Meteorologists generally consider dew point the more reliable measure of how muggy the air actually feels, which is why this calculator's comfort categories key off it instead of the raw humidity percentage.
What does it mean when Frost Risk shows 'Possible overnight'?
It means two things are true at once: the calculated dew point is at or below freezing, so any moisture that condenses will deposit as frost rather than dew, and the air temperature is within about 10 degrees Fahrenheit of that dew point, so overnight cooling could plausibly bring the air down to it. A sub-freezing dew point on its own is not a frost warning — on a dry summer afternoon the dew point can sit near freezing while the air is 50 degrees warmer, and frost is impossible. The spread between the two is what makes the difference.
Why would a weather station's dew point reading differ slightly from this calculator's result?
The Magnus formula used here is a widely accepted meteorological approximation, but real dew point sensors are calibrated instruments that can also account for local air pressure and elevation, which this calculator does not take as inputs. Small differences of a degree or so between a formula-based estimate and an instrument reading are normal and expected.
Related Calculators
The questions that sit next to this one — chosen by subject, including calculators filed under a different category.
Heat Index Calculator
Calculate the heat index (feels-like temperature) based on air temperature and humidity. Assess heat danger level.
Weather & ClimateWind Chill Calculator
Calculate the wind chill temperature using the official NWS formula. Assess frostbite risk based on conditions.
Weather & ClimateHumidity Calculator
Calculate relative humidity from temperature and dew point. Understand comfort levels and weather conditions.
Air QualityMold Risk Calculator
Assess mold growth risk from humidity, temperature, surface type, and ventilation quality with dew point analysis.
HVACPsychrometric Calculator
Calculate wet bulb temperature, dew point, humidity ratio, enthalpy, and specific volume from dry bulb and relative humidity.
More in Environment, Weather & Climate.