Misc A
Misc B
Misc C
Misc D
Misc E
100

water Molecules combine with liquid

condensation

100
How can we measure the amount of water vapor in the atmosphere?

-water vapor pressure

-relative humidity

-Dew Point Pressure

100

condensation equilibrium

evaporation

100

If saturation vapor pressure is 17mb at 15 degrees celsius, about what is it at 5 degrees celsius?

9

100

Decrease in Temperature 

---> eventually reach _______

--->__________

dew point, saturation


200
water molecules break free of liquid

Evaporation

200

small reservoir, but with lots of water movement 

atmosphere


200

ice to water vapor

-without becoming a liquid


Sublimation

200

An increase in temperature leads to....

an increase of saturation vapor pressure= more water vapor can exist

200

Relative Humidity=

%


300

True or False: Nitrogen Pressure is less than water vapor pressure

False


300

Water vapor in the atmosphere

Atmospheric Pressure


300

Water vapor to ice

-without becoming a liquid

Deposition


300

Saturation vapor pressure doubles for every 10 C rise in temp

Rule of Thumb


300

Relative Humidity tells....

how close water vapor pressure is to saturation


400
What are the water vapor pressure units?

mb=milibars

400

evaporation and condensation rates are equal, maximum amount of water vapor present

saturation

400

Saturation vapor pressure depends on....

temperature

400

Rule of Thumb ---> 10 C

18 F

400

temperature you must cool air so that the air is saturated with water vapor

dew point


500

Pressure contributed by water vapor

Water Vapor Pressure

500

Maximum amount of water vapor that can exist

Saturation Vapor Pressure


500

What happens to additional water vapor under saturation vapor pressure?

it condenses


500

10 C(50 F)---> 20 C =

68 F

500

Dew Point Units

C or F

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