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This comprehensive guide explores moisture in the atmosphere, emphasizing its entry primarily from the ocean. We discuss factors affecting evaporation rates such as temperature, surface area, and wind speed. You'll learn about the phases of water in the atmosphere—solid, liquid, and gas—and the concept of evapotranspiration. The importance of measuring humidity, dew point, and the difference between dry and wet bulb temperatures is elaborated upon, highlighting tools and charts for accurate humidity measurement.
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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 – --- • Liquid – --- • Gas - ---
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 - = -
18°C 16°C - = -
Put it all together 20°C 8°C - = - Relative Humidity = %
14°C 10°C - = - Relative Humidity = %
The Dew Point Chart works the same way 14°C 10°C - = - Dew Point = °C
Try These. % °C % °C % °C
% °C % °C °C % °C °C