Dewpoint Formula:
where
\[ \alpha = \frac{a \times T}{b + T} + \ln\left(\frac{RH}{100}\right) \]
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Definition: This calculator estimates the dewpoint temperature based on air temperature and relative humidity using the Magnus formula.
Purpose: It helps meteorologists, HVAC professionals, and others determine when condensation will occur at a given temperature and humidity.
The calculator uses the formula:
where
\[ \alpha = \frac{a \times T}{b + T} + \ln\left(\frac{RH}{100}\right) \]Where:
Explanation: The formula approximates the relationship between temperature, humidity, and the condensation point.
Details: Knowing the dewpoint helps predict fog, frost, and condensation problems in buildings and industrial processes.
Tips: Enter the air temperature in °C, relative humidity (0-100%), and constants a (default 17.27) and b (default 237.7).
Q1: What is dewpoint temperature?
A: The temperature at which air becomes saturated with water vapor and dew forms.
Q2: Why are there constants a and b?
A: These are empirical coefficients in the Magnus formula that vary slightly for different temperature ranges.
Q3: When would I change constants a and b?
A: For temperatures below 0°C, different constants might be more accurate (e.g., a=21.87, b=265.5).
Q4: How accurate is this calculation?
A: It's accurate to within about ±0.4°C for temperatures between -40°C and 50°C.
Q5: What if the RH is 100%?
A: When RH=100%, the dewpoint equals the air temperature (saturated air).