Magnus Formula · Humidity · Weather

Dew Point
Calculator

Calculate dew point from temperature and relative humidity, convert between dew point and RH, and find absolute humidity — using the precise Magnus formula. Supports °F and °C.

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Dew Point Calculator
August-Roche-Magnus approximation
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°C
25°C
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65%
°C
25°C
°C
15°C
°C
25°C
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65%
Comfort Reference

Dew Point Comfort Scale

How different dew point temperatures feel to the human body.

Dry
Comf.
Pleasant
Sticky
Humid
Opp.
Danger
<10°C / <50°F 13°C / 55°F 16°C / 60°F 18°C / 65°F 21°C / 70°F 24°C / 75°F >26°C / >79°F
<10°C / <50°F
🏔️ Very Dry
Arid, desert-like. Skin and lips may feel dry.
10–15°C / 50–59°F
✅ Comfortable
Ideal outdoor conditions. Most people feel comfortable.
15–18°C / 59–65°F
😊 Pleasant
Slightly humid but still comfortable for most people.
18–21°C / 65–70°F
😓 Sticky
Noticeable humidity. Some people feel uncomfortable.
21–24°C / 70–75°F
😰 Oppressive
Very humid. Sweating is less effective at cooling.
>24°C / >75°F
🚨 Dangerous
Extremely oppressive. Heat illness risk in prolonged exposure.
Quick Reference

Dew Point, Temperature & Relative Humidity

Approximate relative humidity at different temperature / dew point combinations.

Air TempDew PointRel. HumidityComfort LevelConditions
35°C / 95°F24°C / 75°F~55%DangerousTropical heat wave; heat stroke risk
30°C / 86°F21°C / 70°F~65%OppressiveTypical summer in southeastern US
28°C / 82°F18°C / 64°F~60%StickyWarm humid summer day
25°C / 77°F15°C / 59°F~55%PleasantComfortable summer conditions
20°C / 68°F10°C / 50°F~52%ComfortableIdeal spring/fall conditions
15°C / 59°F5°C / 41°F~54%ComfortableCool and dry; comfortable jacket weather
10°C / 50°F2°C / 36°F~63%DryCool and mildly humid
10°C / 50°F10°C / 50°F100%FoggyAir fully saturated; fog likely
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Dew Point Is More Reliable Than Relative Humidity

RH changes all day as temperature rises and falls — even if the air's actual moisture content stays exactly the same. On a warm afternoon, RH may drop to 40% while dew point stays at 15°C. Meteorologists use dew point to measure actual moisture because it stays constant unless moisture is added or removed.

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How Dew and Frost Form

Dew forms when a surface cools to the dew point temperature — water vapor in contact with that surface condenses into liquid droplets. This is why grass is wet in the morning even without rain.

When the dew point is below 32°F (0°C), it becomes the frost point — water vapor condenses directly into ice crystals rather than liquid water. Frost can form on surfaces even when air temperature is slightly above freezing, if the surface itself cools below the frost point.

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Dew Point in Weather Forecasting

Meteorologists use dew point as a key forecasting variable. A high surface dew point provides the moisture needed for thunderstorm development. The difference between air temperature and dew point — the "temperature-dew point spread" — is used to forecast fog: when the spread is 5°F (3°C) or less, fog is likely to form.

In severe weather forecasting, surface dew points above 65°F (18°C) are associated with increased severe thunderstorm potential, while dew points above 70°F (21°C) are associated with significant tornado risk in the US.

How Dew Point Is Calculated — The Magnus Formula

The dew point is calculated using the August-Roche-Magnus approximation, one of the most widely used formulas in meteorology and HVAC engineering. It provides accuracy within ±0.4°C for temperatures between −40°C and 60°C, making it suitable for virtually all real-world applications.

Dew Point from Temperature and Relative Humidity

Magnus constants: a = 17.625, b = 243.04°C γ(T, RH) = (a × T) / (b + T) + ln(RH / 100) Dew Point (Td) = (b × γ) / (a − γ) Example: T = 25°C, RH = 65% γ = (17.625 × 25) / (243.04 + 25) + ln(65/100) γ = 440.625 / 268.04 + (−0.4308) γ = 1.6439 − 0.4308 = 1.2131 Td = (243.04 × 1.2131) / (17.625 − 1.2131) Td = 294.89 / 16.41 = 17.97°C ≈ 18°C

Relative Humidity from Temperature and Dew Point

RH = 100 × exp((a × Td) / (b + Td)) ÷ exp((a × T) / (b + T)) Example: T = 25°C, Td = 18°C RH = 100 × exp(17.625×18 / 261.04) ÷ exp(17.625×25 / 268.04) RH = 100 × exp(1.2153) ÷ exp(1.6439) RH = 100 × 3.371 ÷ 5.175 = 65.1%

Absolute Humidity

Absolute humidity is the mass of water vapor per unit volume of air (g/m³). It is calculated from temperature and relative humidity using the Tetens saturation vapor pressure formula:

Saturation vapor pressure: es = 6.1078 × exp(17.27×T / (T + 237.3)) [hPa] Actual vapor pressure: e = es × (RH / 100) Absolute humidity: AH = (e × 2165) / (T + 273.15) [g/m³] Example: T = 25°C, RH = 65% es = 6.1078 × exp(17.27×25 / 262.3) = 31.67 hPa e = 31.67 × 0.65 = 20.59 hPa AH = (20.59 × 2165) / 298.15 = 14.96 g/m³

Dew Point vs Relative Humidity — What's the Difference?

Relative humidity and dew point both measure atmospheric moisture, but they behave very differently — and understanding the difference helps explain why weather apps and meteorologists prefer dew point for comfort assessments.

Why Relative Humidity Changes Through the Day

Relative humidity is the ratio of actual water vapor to the maximum water vapor air can hold at that temperature. Warmer air can hold more water vapor. So as temperature rises through the morning, the air's capacity to hold moisture increases — and relative humidity drops, even though no moisture has left the air. At night when temperature falls, relative humidity rises. A typical summer day might start at 90% RH at dawn and fall to 50% RH by afternoon, with the dew point remaining constant throughout.

Why Dew Point Is a Better Comfort Indicator

Since dew point only changes when actual moisture content changes, it gives a stable, consistent measure of how humid the air truly is — regardless of time of day or temperature. A 70°F dew point feels equally oppressive at 75°F air temperature (95% RH) or at 95°F air temperature (50% RH). In both cases, your body's ability to cool itself by sweating is severely impaired because the air is already heavily loaded with moisture.

Dew Point and Indoor Comfort (HVAC)

In buildings and HVAC engineering, indoor dew point is used to control condensation on surfaces and prevent mold growth. The recommended indoor dew point range is 40–55°F (4–13°C), corresponding to roughly 40–60% relative humidity at typical indoor temperatures of 68–72°F (20–22°C). A dew point above 55°F indoors creates conditions where mold can thrive on cooler surfaces.

Frequently Asked Questions

Dew point is the temperature at which air must be cooled for water vapor to condense into liquid water. It is a direct, absolute measure of moisture in the air — unlike relative humidity, which changes as temperature changes. When air temperature equals the dew point, relative humidity is 100% and fog or dew forms.
The most accurate practical method is the Magnus formula: γ(T,RH) = (a×T)/(b+T) + ln(RH/100), then Td = (b×γ)/(a−γ), where a = 17.625 and b = 243.04°C. This approximation is accurate to within ±0.4°C for temperatures between −40°C and 60°C. Our calculator uses this formula for all three modes.
Relative humidity is the percentage of how saturated the air is — it changes constantly as temperature rises and falls throughout the day, even when actual moisture is constant. Dew point only changes when the actual amount of water vapor in the air changes. A dew point of 15°C always feels the same regardless of air temperature; a 70% RH can feel very different at 20°C vs 35°C.
Below 10°C (50°F): very dry and comfortable. 10–15°C (50–59°F): comfortable. 15–18°C (59–65°F): pleasant. 18–21°C (65–70°F): sticky and noticeable. 21–24°C (70–75°F): oppressive. Above 24°C (75°F): dangerous — heat illness risk during prolonged outdoor activity. The highest dew points ever recorded are around 35°C (95°F) in the Persian Gulf region.
No — dew point can never exceed air temperature. When dew point equals air temperature, relative humidity is exactly 100% and the air is fully saturated. Any further cooling causes condensation (fog, dew, or precipitation). A dew point above air temperature is physically impossible under normal atmospheric conditions.
Because dew point stays constant throughout the day while relative humidity fluctuates with temperature. A day with 90% RH at dawn (cool) and 50% RH at noon (warm) has the same dew point all day — and the body feels the same level of humidity-related discomfort. Meteorologists and forecasters universally prefer dew point as a moisture and comfort indicator for this reason.
Absolute humidity is the mass of water vapor present in a given volume of air, measured in grams per cubic meter (g/m³). Unlike relative humidity (a ratio) or dew point (a temperature), it gives the actual physical quantity of water vapor. At 25°C with 65% RH, absolute humidity is approximately 15 g/m³. It increases with both higher temperature and higher relative humidity.
Dew forms when a surface (grass, car roofs, spider webs) radiates heat overnight and cools to the dew point temperature. Water vapor in the air in contact with that cool surface condenses into liquid droplets. Clear nights with no cloud cover produce the most dew because surfaces can radiate heat efficiently into the sky. Frost forms the same way when the dew point is below 32°F (0°C).
Dew point is critical in forecasting. High surface dew points (above 60°F / 16°C) provide the moisture for severe thunderstorm development. The temperature-dew point spread predicts fog: when spread ≤ 5°F (3°C), fog is likely within hours. Dew points above 70°F (21°C) in the US increase tornado risk significantly. In winter, dew point vs temperature spread helps forecast frost and freezing rain.
The frost point is the temperature at which water vapor condenses directly into ice (frost) rather than liquid water (dew). It is slightly lower than the dew point — when the dew point is below 0°C (32°F), the technically correct term is "frost point." Frost can form on surfaces even when air temperature is slightly above freezing (e.g., 2°C / 36°F), as long as the surface itself cools below the frost point temperature.