Dew Point Calculator

Calculate dew point from air temperature and relative humidity, then review muggy-air comfort, saturation gap, and condensation proximity in one tool.

Last updated: 2026/03/26

Dew Point Calculator

Enter air temperature and relative humidity to estimate dew point, how sticky the air may feel, and how close conditions are to saturation.

Dew point inputs
Live update
Switching the unit also updates the result card and summary table to the same temperature scale.
°F
Recommended range: -22°F to 140°F. This works well for Fahrenheit-first forecast sources.
%
Relative humidity should stay between 1% and 100%. Higher humidity usually pushes dew point upward quickly.
Quick examples
How to read it
  • Dew point is a quick way to read how much moisture is actually in the air, often making cross-day comparisons easier than relative humidity alone.
  • The smaller the gap between the current air temperature and dew point, the closer the air is to saturation, which can make condensation, fog, and muggy air more likely.
  • Actual condensation also depends on surface temperature, radiation cooling, and airflow, so this tool is best used as a fast planning reference.

Enter air temperature and relative humidity to calculate dew point and saturation approach.

Example Remaining spread to saturation 13.0°F · Celsius equivalent 22.7°C
72.9°F
Estimated dew point

At 86°F and 65% relative humidity, dew point is 72.9°F. The overall air feel lands in the very humid band, and the remaining spread to saturation is 13.0°F.

This tool uses the Magnus approximation to estimate dew point from temperature and relative humidity.
Air feel band
Very Humid
Remaining spread to saturation
13.0°F
Condensation approach
Moderate
Formula
Magnus
Dew point comfort bands
DryBelow 50°F · below 10°C
Comfortable50°F to 60°F · 10°C to 16°C
Slightly Humid60°F to 64°F · 16°C to 18°C
Muggy64°F to 70°F · 18°C to 21°C
Very Humid70°F to 75°F · 21°C to 24°C
OppressiveAbove 75°F · above 24°C

Even if air temperature drops later, a high dew point can keep the air feeling sticky and heavy into the evening.

Calculation summary
Input air temperature86.0°F
Relative humidity65.0%
Dew point72.9°F
Remaining spread to saturation13.0°F
Air feel bandVery Humid
Condensation approachModerate
FormulaMagnus approximation
Dew point is a useful weather-planning reference, but actual fog, condensation, and heat stress can still change with surface temperature, radiation cooling, wind, sun exposure, activity level, and health conditions.

What is a Dew Point Calculator?

A Dew Point Calculator turns air temperature and relative humidity into a more intuitive read on how much moisture is actually in the air. Relative humidity can swing a lot when temperature changes, even if the air holds a similar amount of water vapor. Dew point is often easier to compare across days because it reflects the moisture content itself in temperature form.

This version shows dew point, an air-feel band, the remaining spread to saturation, and a condensation-approach cue in one place. That makes it easier to connect the number to practical questions like whether outside air will feel sticky, whether windows may fog more easily, or why evenings still feel heavy after the high temperature starts to fade. If you also want a hot-weather apparent-temperature check, pair it with the Heat Index Calculator.

When this tool is useful

Dew point helps explain muggy air, sticky evenings, and near-saturation conditions in a way that raw humidity percentages often do not. It is especially practical when temperatures swing a lot over the course of a day or when indoor and outdoor conditions differ because of air conditioning.

  • Ventilation decisions — compare whether outside air is likely to feel fresher or more humid than indoor air.
  • Commute and outdoor planning — check whether the air may still feel heavy even after the headline temperature starts to drop.
  • Photo gear or storage planning — watch for conditions that move closer to condensation.
  • Camping, hiking, and fishing — estimate when morning dew, tent moisture, or fog may become more plausible.
  • Sleep comfort checks — explain why a night can feel sticky even when the air temperature looks only moderate.

Key features

Instead of stopping at a single number, this calculator adds interpretation cues that are easier to use in everyday planning.

  • Supports both Celsius and Fahrenheit so you can work directly with local or international forecast sources.
  • Calculates dew point instantly from air temperature and relative humidity.
  • Shows the remaining spread to saturation so you can quickly see how close the air is to condensation conditions.
  • Labels the result with plain-language comfort bands such as Dry, Comfortable, Muggy, and Very Humid.
  • Adds a condensation-approach summary to make the result easier to turn into a real-world judgment.

How to use it

You only need two inputs, but dew point becomes much more useful when you read the number alongside the temperature gap to saturation.

  1. Select Celsius or Fahrenheit to match your forecast source.
  2. Enter the current or expected air temperature.
  3. Enter relative humidity as a percentage.
  4. Read the top result card for dew point and the overall air-feel band.
  5. Use the remaining spread to saturation as a quick cue for how close conditions are to condensation or fog-prone air.

How to interpret dew point

Dew point is the temperature at which air would become saturated if you cooled it without changing its moisture content. That means a higher dew point usually points to more moisture actually present in the air. In practice, dew point often makes muggy-versus-dry comparisons easier than relative humidity alone.

This calculator uses the Magnus approximation, a widely used weather formula for estimating dew point from temperature and relative humidity. As a rough comfort read, values below 50°F often feel fairly dry, 50°F to 60°F tends to feel comfortable, 64°F and above starts to feel muggy for many people, and values above 70°F often feel very humid or oppressive.

The gap between current air temperature and dew point also matters. A smaller gap means the air is closer to saturation, so fog, dew, or condensation can become easier to trigger when a surface cools down or overnight temperatures dip. That does not guarantee fog or condensation by itself, because surface temperature, wind, terrain, and radiation cooling still matter.

If you want to compare hot-season apparent temperature as well, use the Heat Index Calculator. If you want a cold-season apparent-temperature comparison, the Wind Chill Calculator is the better match.

Frequently asked questions

What is the difference between dew point and relative humidity?

Relative humidity shows how close the air is to saturation at the current temperature, while dew point expresses the air’s moisture content as a temperature. Dew point is often easier to compare across different temperatures and times of day.

Why can a high dew point make evenings feel sticky?

A high dew point means the air itself contains a lot of moisture. Even when the air temperature starts to fall, the air may not dry out much, so it can still feel heavy and humid into the evening.

Does a small temperature-dew point gap always mean fog or condensation?

Not always. It means the air is closer to saturation, so condensation or fog becomes easier to trigger if surface cooling, radiation loss, terrain, or other local conditions line up.

What happens if I enter 100% relative humidity?

At 100% relative humidity, the air is essentially saturated, so dew point will be equal to or almost equal to the current air temperature. That means only a small extra temperature drop may be needed for condensation to begin.

Are my inputs stored anywhere?

No. The calculation runs in your browser, and the temperature and humidity values you enter are not stored on the server.

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