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Explore how moisture enters the atmosphere, factors influencing evaporation, measurement techniques for humidity, and the significance of dew point and relative humidity. Learn about evapotranspiration, phases of water in the atmosphere, and tools for determining dew point and relative humidity. Discover the effects of temperature and dew point equality, as well as practical methods for measuring relative humidity.
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Water enters the Atmosphere by A) --- Mainly from Ocean 70% Earth’s surface
Factors Effecting Evaporation Rate a) Surface Temperature Increases ---
b) Surface Area Increases --- Evaporation Evaporation Puddle A Puddle B
c) Humidity increases --- Air is filled with water, no more evaporation. Evaporation Lake
d) Wind Speed Increases -> --- Lake
B) --- Evaporation and Transpiration = Evapotranspiration
Water is found in all phases in the atmosphere • Solid – Clouds, snow • Liquid – Clouds, rain • Gas - Water vapor
Humidity • ---
Relative Humidity • --- • ---
Dew Point • ---
Condensation What happens when the air temperature and dew point are the same?
Sublimation / Deposition FROST SNOW
Tools used to find Dew Point & Relative Humidity • --- • ---
Dew Point & Relative Humidity Charts Best Friend - pg 12
The “Dry Bulb” = Air Temp • Don’t let it fool you. It is just a thermometer. 20°C
The “Wet Bulb” • Has a little wet booty tied to the bottom. • Gets cool when water evaporates. 12°C Wet Booty
14°C 20°C 12°C 8°C A Dry Day… • A lot of moisture will evaporate. • The wet bulb will be a lot cooler than the dry bulb. 20°C Difference between wet bulb & dry bulb is 12 °C.
A Humid Day… • A little bit of moisture will evaporate. • The wet bulb will not be much cooler than the dry bulb. 20°C 14°C Difference between wet bulb & dry bulb is 6 °C.
20°C 14°C 20-14=6
18°C 16°C 18-16=2
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
Try These. % °C % °C % °C
% °C % °C °C % °C °C