Relative Humidity Formula:
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Definition: This calculator estimates the relative humidity based on the dewpoint temperature and air temperature using the Magnus formula.
Purpose: It helps meteorologists, HVAC professionals, and weather enthusiasts determine the humidity level in the air.
The calculator uses the Magnus formula:
Where:
Explanation: The formula calculates how close the air is to saturation by comparing the actual moisture content (represented by dewpoint) to the maximum possible moisture at the current air temperature.
Details: Knowing relative humidity is crucial for weather forecasting, indoor climate control, industrial processes, and human comfort assessment.
Tips: Enter the dewpoint temperature and air temperature in Celsius. Dewpoint cannot exceed air temperature.
Q1: What is dewpoint temperature?
A: The temperature at which air becomes saturated with water vapor and dew begins to form.
Q2: Why can't dewpoint exceed air temperature?
A: Physically impossible - air can't hold more moisture than its saturation point at the current temperature.
Q3: What does 100% RH mean?
A: The air is fully saturated with water vapor - any additional moisture will condense.
Q4: How accurate is this formula?
A: The Magnus formula is accurate to within about ±0.4°C for temperatures between -40°C and 50°C.
Q5: What's a comfortable RH range for humans?
A: Typically 30-60% - lower can cause dryness, higher can feel muggy and promote mold growth.