Earth Science - Atmospheric Moisture

Earth Science - Atmospheric Moisture

Spahn's Science Lectures via YouTube Direct link

EVAPORATION AND CONDENSATION

5 of 17

5 of 17

EVAPORATION AND CONDENSATION

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Earth Science - Atmospheric Moisture

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  1. 1 Intro
  2. 2 WATER'S CHANGES OF STATE: SOLID
  3. 3 LATENT HEAT
  4. 4 PHASE CHANGE DIAGRAM OF WATER
  5. 5 EVAPORATION AND CONDENSATION
  6. 6 SUBLIMATION AND DEPOSITION
  7. 7 HUMIDITY AND SATURATION
  8. 8 THE MIXING RATIO
  9. 9 RELATIVE HUMIDITY AND MOISTURE
  10. 10 RELATIVE HUMIDITY AND TEMPERATURE
  11. 11 DEW POINT TEMPERATURE
  12. 12 HOW IS HUMIDITY MEASURED?
  13. 13 More molecules are returning to the liquid state than are leaving the liquid state. This process is called
  14. 14 As a solid undergoes a phase change to a liquid, it
  15. 15 Which of the following processes absorbs or releases the most heat?
  16. 16 At 25°C it takes 20 grams of water vapor to saturate 1 kilogram of dry air. If there are 5 grams of water vapor in 1 km of air at that temperature, what is the relative humidity?
  17. 17 The temperature at which a dry parcel of air reaches saturation is known as the

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