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Relative Humidity Calculator

Calculate relative humidity from air temperature and dew point. Enter values in Celsius or Fahrenheit and get an instant humidity percentage with useful moisture information.

Calculate Relative Humidity

Temperature Information
Air temperature and dew point must use the same unit.
Calculated Relative Humidity
0
% RH

Enter the air temperature and dew point to calculate relative humidity.

0% 50% 100%
Relative Humidity
Air Temperature
Dew Point
Temp–Dew Point Spread
Waiting for input

What Is a Relative Humidity Calculator?

A Relative Humidity Calculator estimates the percentage of moisture in the air relative to the maximum amount of water vapor the air could hold at the same temperature.

This calculator uses air temperature and dew point to determine relative humidity. Because the amount of water vapor that corresponds to saturation changes with temperature, relative humidity is temperature dependent.

Quick definition: Relative humidity is the ratio of actual water-vapor pressure to saturation water-vapor pressure at the same temperature, expressed as a percentage.

How to Use the Relative Humidity Calculator

The calculator requires two values: the current air temperature and the dew point temperature.

1

Enter Air Temperature

Enter the measured air temperature for the conditions you want to calculate.

2

Enter the Dew Point

Enter the dew point using the same temperature unit as the air temperature.

3

Calculate Relative Humidity

Select Celsius or Fahrenheit and click the button to calculate the estimated relative humidity percentage.

How Is Relative Humidity Calculated?

Relative humidity can be estimated from air temperature and dew point by comparing the saturation vapor pressure at the dew point with the saturation vapor pressure at the air temperature.

Relative Humidity Formula

RH = 100 × [e(Td) ÷ e(T)]

e(T) = exp[(17.625 × T) ÷ (243.04 + T)]

Here, T represents air temperature in Celsius and Td represents dew point in Celsius. If Fahrenheit values are entered, the calculator converts them to Celsius before performing the calculation.

Relative Humidity Calculation Example

Suppose the air temperature is 25°C and the dew point is 15°C. Using the vapor-pressure relationship gives a relative humidity of approximately 54%.

If the air temperature decreases while the amount of water vapor remains similar, relative humidity generally rises. When the air temperature reaches the dew point, relative humidity approaches 100%.

Helpful relationship: When air temperature and dew point are close together, relative humidity is usually high. A larger difference generally indicates lower relative humidity.

Relative Humidity vs. Dew Point

Relative humidity and dew point are both related to atmospheric moisture, but they describe moisture in different ways.

Measurement What It Describes Unit
Relative Humidity Moisture relative to saturation at the current air temperature %
Dew Point Temperature at which the air reaches saturation when cooled under the assumed conditions °C or °F
Air Temperature Current thermal condition of the air °C or °F

What Affects Relative Humidity?

Air Temperature

Relative humidity changes as air temperature changes, even when the actual water-vapor amount remains approximately constant.

Water Vapor

Adding or removing water vapor directly changes the moisture content of the air and therefore affects relative humidity.

Dew Point

Dew point provides information about atmospheric moisture and can be combined with temperature to estimate relative humidity.

Air Exchange

Ventilation and movement of air between spaces with different moisture conditions can change indoor humidity.

Understanding Relative Humidity Results

Relative humidity ranges from approximately 0% for extremely dry air toward 100% as air approaches saturation. The meaning of a particular value depends on temperature and the application being considered.

Relative Humidity General Description
Below 30% Low relative humidity
30%–40% Moderate-low humidity
40%–60% Moderate relative humidity
60%–80% High relative humidity
Above 80% Very high relative humidity
100% Air is at saturation under the measured conditions
Important: Relative humidity alone does not tell you the total amount of water vapor in the air. Temperature must also be considered when comparing different conditions.

Why Is Relative Humidity Important?

Weather

Relative humidity is widely used in weather observations because it provides information about how close the air is to saturation at its current temperature.

HVAC and Buildings

Humidity measurements can help evaluate indoor environmental conditions, ventilation, dehumidification, humidification, and potential condensation concerns.

Storage and Manufacturing

Some materials and products are sensitive to moisture. Humidity monitoring can therefore be important in storage areas, laboratories, manufacturing facilities, and other controlled environments.

Agriculture

Temperature and humidity can influence plant environments, evaporation, greenhouse management, and other agricultural processes.

Relative Humidity Calculator FAQs

Relative humidity is the ratio between the actual water-vapor pressure and the saturation water-vapor pressure at the same temperature, expressed as a percentage.

Relative humidity can be estimated by calculating saturation vapor pressure at the dew point and dividing it by saturation vapor pressure at the current air temperature. This calculator performs those steps automatically.

A relative humidity of 100% means the air is at saturation for the measured temperature and pressure conditions.

Yes. Enter both air temperature and dew point in Fahrenheit and select the Fahrenheit option. The calculator handles the internal conversion automatically.

When the air temperature equals the dew point, the air is at or very near saturation and relative humidity is approximately 100%.

Under ordinary unsaturated atmospheric conditions, dew point should not be higher than the current air temperature. If it is, the measurements or inputs should be checked.

The saturation vapor pressure of water changes strongly with temperature. Because relative humidity compares actual vapor pressure with saturation vapor pressure, changing temperature can change relative humidity even without adding or removing much water vapor.