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Atmospheric Chemistry > Relative Humidity
The following information is about Relative Humidity.
Relative Humidity Defined
This is the ratio between the actual water vapor content of the atmosphere and the maximum water vapor content possible at that given temperature. If the temperature of a given parcel of air rises, the amount of moisture it can hold increases and as such its relative humidity decreases. If there is no change in temperature but the moisture content decreases then the relative humidity will again decrease because the ratio of actual water vapor present is less than the maximum amount the air could hold. Conversely, if the water content does not change but the temperature falls, the relative humidity increases until saturation and possible precipitation occurs. [Ocean; v17; p34-6; 1984.] [Science News; v132; p236; 1987.]
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Off-site Relative Humidity Links, User Submitted
The following links have been collected through user bookmark submission in the Relative Humidity category. Please note, because these resources are off-site we cannot guarantee the accuracy or quality of any information.
Wed Oct 29
- Gibraltar Weather Thursday October 30th 2008: Gibraltar Weather 5 five day forecast 20°C W (16 mph) Relative Humidity 66%, Pressure 1011mB, Rising Visibility: Very Good
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Wed May 7
- Sensirion - Relative Humidity Sensors and Temperature Humidity Control: Sensirion AG - the leading sensor manufacturer. We provide relative humidity sensors and flow sensor solutions with unique performance. Together with our capacitive humidity sensor...
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Thu Jan 3
- Relative Humidity Calculator, Relative Humidity Calculation: Relative Humidity Calculator, Relative Humidity Calculation
Thu Oct 11
- National Weather Service - NWS Sacramento: relative humidity tables
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