Dew Point Calculation:
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The dew point temperature is the temperature to which air must be cooled to become saturated with water vapor. It's a measure of atmospheric moisture and indicates the temperature at which dew or frost will form.
The calculator uses the following equations:
Where:
Explanation: The first equation calculates vapor pressure from wet and dry bulb temperatures, then the second equation converts this to dew point temperature.
Details: Dew point is crucial in meteorology, HVAC design, industrial processes, and agriculture. It helps predict fog, frost, and human comfort levels.
Tips: Enter wet bulb and dry bulb temperatures in °C, and station pressure in hPa. All values must be valid (pressure > 0).
Q1: What's the difference between dew point and wet bulb temperature?
A: Wet bulb temperature is the lowest temperature air can reach by evaporative cooling, while dew point is the temperature at which air becomes saturated.
Q2: What is a comfortable dew point range?
A: Below 16°C (60°F) is comfortable, 16-18°C (60-65°F) is somewhat humid, above 18°C (65°F) is uncomfortable.
Q3: Why is station pressure important?
A: Pressure affects the relationship between temperature and humidity. The calculation requires local station pressure for accuracy.
Q4: Can I use this for high altitude calculations?
A: Yes, as long as you use the correct station pressure for your altitude.
Q5: What's the saturation vapor pressure formula?
A: \( e_s = 6.112 \times \exp\left(\frac{17.67 \times T}{T + 243.5}\right) \) where T is temperature in °C.