InputsLive
Air temperature
°C
Dew point
°C
Dew point must be ≤ air temperature.
Result
Relative humidity
53.8%
Comfortable · dew point 15°C
Relative humidity53.8%
ComfortComfortable
Air temp25°C
Dew point15°C

Relative humidity via inverse Magnus formula (Sonntag 1990). Dew point must be ≤ air temperature.

Results are estimates. Consult a professional.

What it measures

What is relative humidity?

Relative humidity is the amount of water vapor the air is holding compared with the most it could hold at its current temperature, written as a percentage. At 60% relative humidity the air is carrying 60% of its maximum moisture for that temperature; at 100% it is saturated and water begins to condense. This relative humidity calculator takes an air temperature and a dew point and returns the relative humidity that pairs with them.

The "relative" part is the catch. Because warm air can hold far more vapor than cold air, the same physical amount of moisture reads as a high humidity on a cool morning and a much lower humidity by a warm afternoon — even though no water entered or left the air. That is why a single relative humidity figure only makes sense once you know the temperature it was measured at.

How it's calculated

How the relative humidity calculator works

The calculator inverts the Magnus formula. The Magnus relation links three quantities — air temperature, dew point, and relative humidity — so given any two it can solve for the third. Here you supply the air temperature and the dew point, and the calculator returns the relative humidity directly, with no intermediate steps to track.

R = 100 × exp( (17.625 × Td)/(243.04 + Td) (17.625 × T)/(243.04 + T) )
The coefficients used here (a = 17.625, b = 243.04 °C) are the Sonntag (1990) Magnus-form values. For the underlying meteorological convention — that dew point is the temperature at which relative humidity reaches 100% — see the U.S. National Weather Service.
The two inputs

The inputs explained

Two readings go in, and both are everyday weather values. Knowing how each one moves the result makes the relative humidity easy to reason about.

Air temperature

The ordinary dry-bulb temperature from a thermometer or weather report, entered in °C. It sets the air's moisture capacity: at a fixed dew point, a warmer air temperature means a lower relative humidity, because the warmer air could hold more than it currently is.

Dew point

The temperature to which the air would have to cool before its moisture condenses, also in °C. It fixes the actual water content. The closer the dew point sits to the air temperature, the higher the relative humidity — and when the two are equal, the air is saturated and humidity reads 100%.

Example

A worked example using the relative humidity calculator

Example: a mild room at 25 °C with a 15 °C dew point

A hygrometer reads an air temperature of 25 °C (77 °F) and a dew point of 15 °C (59 °F). Those are the calculator's default inputs. The dew point alone says the air is moderately moist, but to know whether the room sits in the comfortable band you need the relative humidity.

Step 1 — Enter the two readings

Air temperature 25 °C, dew point 15 °C. The dew point is below the air temperature, as it must be, so the result will land below 100%.

Step 2 — Evaluate the two Magnus terms

The dew-point term is (17.625 × 15) / (243.04 + 15) = 1.0246 and the temperature term is (17.625 × 25) / (243.04 + 25) = 1.6439. Their difference, the exponent, is −0.6193.

Step 3 — Solve for the relative humidity

Exponentiating and scaling gives R = 100 × exp(−0.6193) = 53.8%.

53.8% relative humidity — comfortable
At 53.8% the room sits inside the 40–60% comfort band most people prefer. Hold the dew point at 15 °C but warm the room to 30 °C and the relative humidity falls to about 40%; cool it to 20 °C and it climbs to roughly 73%. The moisture never changed — only the temperature, and with it the air's capacity, did.
Comfortable indoor RH

What is a comfortable indoor humidity?

For occupied indoor spaces, a relative humidity of roughly 40–60% is the range most people find comfortable and that limits the problems at either extreme — dry air and static below it, mustiness and mold above it. The table below shows what happens as you move through the bands.

Indoor relative humidityHow it feelsWhat to expect
Below 30%Too dryDry skin, chapped lips, irritated airways, and frequent static shocks; wood floors and furniture can crack.
30–40%Dry but acceptableComfortable for most people; a humidifier helps in winter if static or dry sinuses appear.
40–60%ComfortableThe target band — air feels neither dry nor clammy, and mold and dust-mite growth are kept in check.
60–70%Slightly humidAir starts to feel sticky; condensation appears on cold windows and mold risk begins to rise.
Above 70%Too humidPersistent dampness, condensation, and a real risk of mold, mildew, and dust-mite proliferation.

The 40–60% target follows ASHRAE guidance for occupied spaces; the upper limit aligns with the EPA's advice to keep indoor humidity below 60% (cited below). Individual comfort varies with temperature, clothing, and activity.

RH vs dew point

Relative humidity vs dew point: which to trust

Relative humidity is intuitive indoors, where temperature is roughly steady, but it is a poor way to compare moisture across different temperatures. Because the percentage is measured against a ceiling that rises and falls with temperature, the same air can post wildly different relative humidity numbers through a single day while its actual water content never moves.

One dew point, two relative humidities
Air with a steady 15 °C dew point reads 73% relative humidity at 20 °C but only 40% at 30 °C. Nothing was added or removed — the warmer air simply has more room, so the same moisture fills a smaller share of it. The dew point, fixed at 15 °C, tells the honest story.

For judging how muggy outdoor air will feel, the dew point is the more reliable gauge precisely because it does not drift with temperature. The U.S. National Weather Service makes the same point: to compare how humid two days feel, look at the dew point rather than the relative humidity. If you have the temperature and humidity instead, the dew point calculator runs the conversion the other way.

National Weather Service (La Crosse, WI) — guidance that the dew point, not relative humidity, is the better indicator of how humid the air feels because relative humidity shifts with temperature.
Health thresholds

Humidity, mold, static, and health thresholds

The 40–60% band is not only about comfort — it is where the main moisture-related risks are smallest. The EPA advises keeping indoor relative humidity below 60%, and ideally between 30% and 50%, because relative humidity above 60% promotes condensation and mold growth.

  • Above 60% — mold and dust mites. Sustained high humidity lets mold, mildew, and dust mites flourish on walls, fabrics, and around windows. The EPA names 60% as the line to stay under for mold control.
  • Below 30% — dry-air effects. Very dry air dries out skin and airways, worsens static electricity, and can crack wood. It also helps some airborne viruses persist, which is why winter indoor air often feels harsh.
  • 40–60% — the sweet spot. Inside this band, mold and mite growth slow, static eases, and most people breathe comfortably. It is the band ASHRAE recommends for occupied spaces and the one to aim a humidifier or dehumidifier at.
U.S. Environmental Protection Agency — "A Brief Guide to Mold, Moisture and Your Home": keep indoor humidity below 60 percent relative humidity (ideally between 30 and 50 percent) to control mold.
Common mistakes

Common relative humidity mistakes to avoid

  • Comparing humidity readings at different temperatures. A 70% reading in a cool basement and a 50% reading in a warm living room can hold similar moisture. Compare dew points, not raw percentages, when temperatures differ.
  • Assuming high humidity means a lot of water in the air. Cold air at 90% relative humidity holds little moisture in absolute terms. The percentage describes how full the air is, not how much water it carries.
  • Forgetting that heating dries the air. Warming a room without adding moisture raises its capacity and drops the relative humidity — the reason indoor air turns dry and static-prone in winter even when outdoor humidity is high.
  • Treating the comfort band as exact. The 40–60% range is guidance, not a hard line. A reading of 62% is not a crisis; a persistent 75% is the real signal to run a dehumidifier.

For related views of the same moist air, the heat index calculator shows how hot high humidity makes it feel, and the dew point calculator converts temperature and humidity into the absolute moisture measure.

Accuracy

How accurate is this relative humidity calculator?

The calculator uses the inverse Magnus formula with the Sonntag (1990) coefficients (a = 17.625, b = 243.04 °C), the standard way to relate temperature, dew point, and relative humidity. Across the everyday range of −40 to +50 °C the Magnus relation is accurate to within a fraction of a percent of relative humidity — far tighter than any home hygrometer. The result is clamped to 0–100%, so a dew point entered above the air temperature returns 100% rather than an impossible value.

The arithmetic is reliable; the inputs are the weak link. A dew point taken from a cheap sensor, or two readings measured minutes and meters apart, will shift the humidity. And the comfort and health bands are general guidance — acclimation, airflow, and activity all change how a given humidity feels. Treat the percentage as a solid number and the comfort labels as rules of thumb.

Questions

Frequently asked questions about the free relative humidity calculator

A humidity calculator is a free online tool that helps you find relative humidity from air temperature and dew point — the inverse Magnus formula. Relative humidity is the ratio of actual water vapor to the maximum the air could hold at that temperature, expressed as a percentage. It can be computed from air temperature and dew point using the inverse of the Magnus formula. It runs entirely in your browser with instant results and no sign-up.
ASHRAE recommends 40-60% RH for occupied spaces. Below 30% causes dry skin and static; above 60% accelerates mold growth and feels muggy.
RH depends on temperature, so the same actual moisture gives different RH numbers at different temperatures. Dew point measures absolute moisture and stays constant as temperature changes.
Not in normal practice. RH > 100% means supersaturation, which is unstable — moisture immediately condenses. The calculator clamps to 100%.
About

About this relative humidity calculator

This relative humidity calculator runs entirely in your browser — nothing you enter is sent anywhere. It solves relative humidity from the air temperature and dew point with the inverse Magnus formula and reports the result as a percentage, clamped to a physical 0–100% range.

It pairs with the dew point calculator and the heat index calculator. Browse every weather tool on the calculators index.

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