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Dew Point & Relative Humidity. How to use a Psychrometer. Water in the Atmosphere. Humidity : measure amount of water vapor stuck between molecules in atmosphere; air’s ability to hold water depends on the air temp The hotter the air, the more water the air can hold
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Dew Point & Relative Humidity How to use a Psychrometer
Water in the Atmosphere • Humidity: measure amount of water vapor stuck between molecules in atmosphere; • air’s ability to hold water depends on the air temp • The hotter the air, the more water the air can hold • Relative humidity: amount of water vapor (%) present compared to total amount air can hold at a given temperature • If relative humidity is 100% then precipitation is occurring • Dew Point – temperature at which RH = 100% • If dew point = actual temperature then precipitation is occurring
The “Dry Bulb” • Don’t let it fool you. It is just a thermometer. • measures air temperature
The “Wet Bulb” • wet “sock” tied to bulb (called ‘wick’) • cools as water evaporates
14°C 20°C 12°C 8°C A Dry Day… • lots of moisture evaporates • wet bulb will be much cooler than dry bulb 20°C Difference between wet bulb & dry bulb is 12 °C.
A Humid Day… • little moisture will evaporate • wet bulb will be slightly cooler than dry bulb 20°C 14°C Difference between wet bulb & dry bulb is 6 °C.
Finding Dew Point and Relative Humidity • Warning #1: Be sure to READ the correct chart: DPT or RH • Warning #2: Dew Point Temperature IS NOT “Difference between wet bulb and dry bulb”. • Warning #3: The wet bulb temp IS NOT the DPT.
20°C 14°C 20-14=6
Put it all together 20°C 8°C 20-8=12 Relative Humidity = 11%
14°C 10°C 14-10=4 Relative Humidity = 60%
The Dew Point Chart works the same way 14°C 10°C 14-10=4 Dew Point = 6°C