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Calcimator

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

Dew Point Unit°F
Comfort LevelCold — comfort scale does not apply
Temp/Dewpoint Spread10.8°
Frost RiskNo — dew point is below freezing but the air is far too warm to reach it

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
  1. Select your Temperature Unit (Fahrenheit or Celsius).
  2. Enter the Air Temperature.
  3. Set the Relative Humidity (%).
  4. Review the Dew Point temperature, Comfort Level, Temp/Dewpoint Spread, and Frost Risk indication.

How the result changes with Air Temperature

Air TemperatureDew Point
2010.2
3019.7
5442.5

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

  1. Identify Input Parameters
    3 parameters
    Temperature Unit = 0, Air Temperature = 40, Relative Humidity = 65 = 3 input(s) provided
  2. Calculate Dew Point
    Td = (b x alpha) / (a - alpha), alpha = (a x T)/(b + T) + ln(RH/100)
    29.2 = 29.2
  3. Calculate Comfort Level
    Comfort Level = band lookup on dew point in degC
    Cold — comfort scale does not apply = Cold — comfort scale does not apply
  4. Calculate Temp/Dewpoint Spread
    Temp/Dewpoint Spread = round((displayTemp - displayDewPoint) * 10) / 10
    10.8 = 10.8

Figures and sources

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.

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