Time & Date Planning
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Calculate dew point temperature from air temperature and humidity
Dew point is the temperature at which air becomes saturated with moisture and water vapor begins to condense into liquid water (dew). It's a direct measure of the amount of moisture in the air and is a better indicator of comfort than relative humidity.
The Magnus-Tetens approximation formula:
Td = (b × α(T,RH)) / (a - α(T,RH))
Where α(T,RH) = (a × T)/(b + T) + ln(RH/100)
Constants: a = 17.27, b = 237.7°C for temperatures above 0°C
The difference between air temperature and dew point (temperature spread) indicates how close the air is to saturation:
Relative humidity is a percentage that changes with temperature, while dew point is an absolute measure of moisture in the air. Dew point doesn't change with temperature, making it a more reliable indicator of actual moisture content and comfort level.
No, dew point can never be higher than the current air temperature. When air temperature equals the dew point, the air is 100% saturated (100% relative humidity), and condensation occurs.
As temperatures drop overnight, the air temperature can reach the dew point. When surfaces cool below the dew point temperature, water vapor in the air condenses on those surfaces, forming dew. This is most common on clear, calm nights.
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