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Dew Point Calculator

Find dew point from air temperature and relative humidity, compare comfort ranges, build tables, and export CSV.

Dew Point Humidity Unit Conversion Table Export

Dew Point Estimator & Table Builder

Enter temperature and humidity to calculate dew point in °C/°F with interpretation, optional absolute humidity estimate, and CSV export.

Dew point comfort guide (common rule of thumb):
  • < 10°C (50°F): dry, comfortable for most people
  • 10–16°C (50–60°F): comfortable to slightly humid
  • 16–21°C (60–70°F): humid, noticeable stickiness
  • 21–24°C (70–75°F): very humid, uncomfortable for many
  • > 24°C (75°F): oppressive humidity

What a Dew Point Calculator Tells You

A Dew Point Calculator estimates the dew point temperature from air temperature and relative humidity. Dew point is the temperature at which air becomes saturated with water vapor. If air cools to that point, excess moisture must condense, forming dew on surfaces, fog near the ground, or condensation on windows and pipes.

Dew point is often more informative than relative humidity for everyday comfort because it tracks moisture content more directly. Relative humidity can swing up or down just because temperature changes, even if moisture stays constant. Dew point, in contrast, provides a stable “how much moisture is actually in the air” indicator.

Dew Point vs Relative Humidity

Relative humidity (RH) is the percentage of water vapor in the air compared to the maximum the air could hold at that temperature. Warm air can hold more water vapor than cool air, so the same amount of moisture yields a lower RH at higher temperatures and a higher RH at lower temperatures. That is why RH alone can feel confusing.

Dew point solves that confusion by expressing moisture content as a temperature. The closer dew point is to air temperature, the more saturated the air is. When RH reaches 100%, dew point equals the air temperature and condensation can form easily.

How Dew Point Is Calculated

Meteorology often uses simplified formulas that approximate water vapor saturation pressure and convert RH into dew point. This tool includes two common approaches:

  • Magnus (standard approximation used widely for weather calculations)
  • Arden Buck (a refined saturation vapor pressure approximation that can improve accuracy in some ranges)

Both methods follow the same idea: compute a “humidity term” using temperature and RH, then solve for the dew point that corresponds to the same vapor pressure.

Concept (Magnus-style)
γ(T,RH) = (a·T / (b + T)) + ln(RH/100)
DewPoint = (b·γ) / (a − γ)

In this model, T is temperature in °C, RH is relative humidity in percent, and a and b are empirical constants chosen to fit atmospheric behavior. The calculator handles unit conversion automatically if you enter temperature in °F.

Why Dew Point Matters for Comfort

Dew point is strongly linked to how humid the air feels because it reflects moisture content. Higher dew points mean sweat evaporates more slowly, which makes warm weather feel stickier and more exhausting. Lower dew points mean drier air, which improves evaporation and makes hot temperatures feel more tolerable.

Many people find dew point easier to interpret than RH. A dew point of 12°C might feel comfortable even at high temperatures, while a dew point of 24°C can feel oppressive even if the air temperature is not extreme.

Condensation, Fog, and Indoor Moisture

Dew point is also important for predicting condensation. If a surface is colder than the dew point of the surrounding air, water vapor can condense on that surface. This is why dew point is relevant for:

  • Fog formation near the ground
  • Dew on grass and cars in the morning
  • Condensation on windows, pipes, and air-conditioning vents
  • Mold risk in buildings with poor ventilation

Indoors, monitoring dew point can help you manage comfort and reduce condensation risk. For example, if indoor dew point is high, a cold air-conditioned surface may condense moisture and drip. Dehumidification reduces dew point and helps prevent that.

Absolute Humidity (Optional Estimate)

Absolute humidity is the mass of water vapor per volume of air (often expressed in g/m³). While dew point is often the most practical number for comfort, absolute humidity is useful in some engineering and indoor air quality contexts. This calculator can estimate absolute humidity based on temperature and RH using standard vapor pressure relationships.

This value is an estimate because it depends on assumptions such as pressure near sea level. For everyday use, dew point is usually the more actionable metric.

How to Use the Dew Point Calculator

  • Enter air temperature in °C or °F.
  • Enter relative humidity (0–100%).
  • Choose Magnus (standard) or Arden Buck (refined).
  • Optionally display absolute humidity.
  • Click calculate to see dew point in °C and °F plus a comfort label.

The step table shows conversions and intermediate terms so you can understand the process and verify inputs. If you want multiple values at once, the table builder creates a dew point grid across a temperature range and humidity range and exports it to CSV.

Dew Point vs Heat Index

Dew point and heat index are related but not identical. Dew point measures moisture content directly. Heat index estimates perceived heat stress from temperature and humidity combined. In hot weather, high dew point often explains why heat index rises sharply: humidity limits evaporation and makes heat feel worse. That said, dew point can be high even when temperatures are moderate, making it a good “humidity feel” metric year-round.

Limitations and Assumptions

Dew point calculations are only as good as the inputs. Sensor placement, sun exposure, and microclimates can influence reported temperature and humidity. The formulas used here are approximations that are widely used and generally accurate in typical atmospheric ranges, but extreme conditions can introduce small differences. For most everyday weather, comfort, and planning decisions, these estimates are more than sufficient.

FAQ

Dew Point Calculator – Frequently Asked Questions

Answers about dew point meaning, humidity differences, comfort interpretation, condensation, formulas, and table exports.

Dew point is the temperature at which air becomes saturated with water vapor. If air cools to the dew point, condensation (dew or fog) can form.

Not exactly. Relative humidity depends on temperature, while dew point measures the actual moisture content more directly. Higher dew point means more moisture in the air.

This tool uses a standard Magnus-type dew point approximation (commonly used in meteorology) and returns dew point in both °C and °F.

High dew points indicate humid air that reduces sweat evaporation, making it feel sticky and warmer. Lower dew points feel drier and more comfortable.

In typical outdoor conditions, dew point is at or below the air temperature. Dew point equals air temperature at 100% relative humidity.

As a rule of thumb: below ~10°C (50°F) feels dry, 10–16°C (50–60°F) is comfortable, 16–21°C (60–70°F) feels humid, and above ~21°C (70°F) feels very humid.

Yes. Build a dew point grid across a temperature range and humidity range, then export it to CSV.

Dew point measures moisture content; heat index estimates “feels like” heat stress from temperature and humidity. Dew point helps explain why heat index can be high.

The result is an estimate based on a widely used approximation. Accuracy is typically strong for common atmospheric ranges, but extreme conditions and sensor errors can affect inputs.

Dew point and absolute humidity results are estimates based on standard meteorological approximations. Real-world comfort can differ due to wind, sun exposure, acclimatization, and local microclimates.