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Dew Point vs Relative Humidity Calculator

Compare the dew point and relative humidity calculators: two moisture measures of the same air, computed from different inputs, and when to use which.

Dew point and relative humidity describe the same moisture state of the air from two different angles, and the two calculators are inverses of each other. Dew point is the temperature at which the current air would become saturated if cooled at constant moisture — a direct measure of how much water vapor is actually present. Relative humidity is the ratio of the actual vapor pressure to the saturation vapor pressure at the current air temperature — a measure of how close the air is to saturation. A warm afternoon and a cool morning can have very different relative humidity but nearly the same dew point, which is why the choice between the two tools comes down to which quantity you already have and which question you are answering.

What each calculator does

The dew point calculator takes air temperature and relative humidity, converts Fahrenheit inputs to Celsius, and applies the Magnus approximation with constants a = 17.27 and b = 237.7:

γ=a×Tb+T+ln(RH100),Td=b×γaγ\gamma = \frac{a \times T}{b + T} + \ln\left(\frac{RH}{100}\right), \qquad T_{\text{d}} = \frac{b \times \gamma}{a - \gamma}

The result appears in the selected unit and also lists the dew point in Celsius, rounded to two decimals. It is useful for weather interpretation, HVAC troubleshooting, greenhouses, storage rooms, and any situation where moisture becomes a problem only after a surface gets cold enough: condensation can occur when a surface is at or below the dew point.

The relative humidity calculator takes air temperature and dew point (rejecting a dew point above the air temperature), converts to Celsius, and applies the Magnus-Tetens relationship with constants 17.625 and 243.04:

RH=100×exp(17.625×Td243.04+Td)exp(17.625×T243.04+T)RH = 100 \times \frac{\exp\left(\frac{17.625 \times T_{\text{d}}}{243.04 + T_{\text{d}}}\right)}{\exp\left(\frac{17.625 \times T}{243.04 + T}\right)}

The displayed result is clamped between 0 percent and 100 percent, rounded to two decimals, and labeled positive only in the 30 percent through 60 percent comfort band used by the page — the range commonly cited for indoor comfort and moisture control.

Side-by-side

Dew point calculatorRelative humidity calculator
InputsAir temperature and relative humidityAir temperature and dew point
OutputDew point temperature in the selected unit plus CelsiusRelative humidity percentage, 0–100%
FormulaMagnus approximation (a = 17.27, b = 237.7)Magnus-Tetens vapor-pressure ratio (17.625, 243.04)
What it measuresActual water vapor contentCloseness to saturation at current temperature
Comfort useOutdoor mugginess; condensation when surfaces reach the dew pointIndoor comfort band of 30%–60%; mold and moisture control
Display roundingTwo decimalsTwo decimals, clamped 0–100%
RejectsZero percent humidity produces a non-useful logarithmDew point above air temperature

When to use which

Use the dew point calculator when you have temperature and relative humidity and want the dew point — for example, to anticipate condensation on a window, pipe, wall, or stored material, or to compare how muggy two days are with a number that does not shift every time the temperature changes. Use the relative humidity calculator when you have temperature and dew point and want the percentage — for example, to check a room against the 30 percent to 60 percent indoor comfort band or to understand how close the air is to saturation.

The two tools describe the same air, so use both when comfort, condensation, and heat stress all matter. In hot conditions, pair either result with the heat index calculator for heat-stress context. Do not mix observations from different times or places: both formulas assume the temperature and the moisture reading describe the same parcel of air.

Limits and disclaimer

Both pages are educational tools. The comfort figures are rules of thumb, not official medical limits — dew point comfort depends on acclimation, wind, sun, and activity, and mold risk depends on surface temperature, wetting duration, leaks, ventilation, and materials, not the room-air percentage alone. The Magnus approximations are accurate for common weather and indoor conditions but not for industrial drying, cryogenic temperatures, compressed-air systems, or precision psychrometrics, which may need full thermodynamic calculations and calibrated instruments.

Try them

Frequently asked questions

Which calculator should I use if I have temperature and relative humidity?
Use the dew point calculator: it converts air temperature and relative humidity into the dew point temperature with the Magnus approximation. If instead you have temperature and dew point, use the relative humidity calculator, which converts those into a relative humidity percentage. The two tools are inverses, so the one to use depends on which quantity you know and which you need.
Why do the two pages use different formulas?
Each page implements the conversion in the direction it needs. The dew point calculator applies the Magnus approximation with constants a = 17.27 and b = 237.7 to solve for dew point from temperature and relative humidity. The relative humidity calculator applies the Magnus-Tetens relationship with constants 17.625 and 243.04 to estimate the vapor-pressure ratio from temperature and dew point. Both are accurate enough for ordinary weather and indoor conditions but remain approximations.
Which measure is better for describing how muggy it feels?
For comparing outdoor days, dew point is often more intuitive because it tracks the actual water vapor content and changes less when the air warms or cools; dew points in the low 60s Fahrenheit feel noticeably humid and the low 70s oppressive to many people. Relative humidity is more useful indoors, where saturation matters for condensation and mold: the relative humidity calculator labels 30 percent through 60 percent as the comfortable band. Use both when comfort, condensation, and heat stress all matter.

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