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Ch. 27: Evaporation, Condensation, and Precipitation

Ch. 27: Evaporation, Condensation, and Precipitation. I. Evaporation & Humidity A. Water’s changing states: 1. Solid  liquid = melting 2. Liquid  gas = evaporation 3. Gas  liquid = condensation. Evaporation:

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Ch. 27: Evaporation, Condensation, and Precipitation

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  1. Ch. 27: Evaporation, Condensation, and Precipitation

  2. I. Evaporation & Humidity A. Water’s changing states: 1. Solid  liquid = melting 2. Liquid  gas = evaporation 3. Gas  liquid = condensation

  3. Evaporation: • 1. Heat is absorbed from the environment in this process, so it is a cooling process.

  4. Phases of Matter Gas Liquid Solid

  5. C. Relative Humidity - compares the amount of water in the air with the maximum amount it can hold at that temperature. Rel. Humidity = mass of water in air X 100 mass of water air can hold

  6. 1. Measured with a psychrometer - basically 2 thermometers together, where 1 has a wet cotton sleeve over its bulb.

  7. 2. You make two measurements… the dry bulb temp. & the wet bulb temp.

  8. 3. Use those values in your Reference Tables to find the relative humidity.

  9. What is the relative humidity if the dry bulb temp is 12 C and the wet bulb temp is 8 C

  10. What is the relative humidity if the dry bulb temp. is 26 C and the wet bulb is 24 C? 85%

  11. What is the relative humidity if the dry bulb temp. is 20 C and the wet bulb is 11 C? 30%

  12. If the dry bulb temperature is 14 C and the relative humidity is 79%, what is the wet bulb temperature? 12 C

  13. II. Forms of Condensation A. When the air temperature drops so that it can no longer hold the amount of water vapor it contains, the water condenses on objects outdoors. This is called dew.

  14. B. The temperature at which this will occur is called the dew point. 1. Measured just like humidity with a psychrometer. 2. A separate Reference Table lets us calculate this value.

  15. C. Requirements for condensation: (cooling air!) Ways air can be cooled: 1. A cold surface 2. radiated heat 3. Mixing with colder air 4. Expanding as it rises

  16. a. You must have something for the water to condense upon! These little particles in the atmosphere are called condensation nuclei.

  17. D. When condensation freezes, it forms frost. E. Condensation can be visible in the air as fog. 1. Radiation fogs - ground cools rapidly at night, forming a cool layer of air near the ground. 2. Advection fogs - warm, moist southerly winds blow over snow-covered ground, forming fog.

  18. What is the dewpoint temp. if the dry bulb temp is 22 C and the wet bulb temp is 20 C? 19 C

  19. If the dry bulb temperature is 0 C and the dewpoint temp is -9 C, what is the wet bulb temp? -3 C

  20. III. Clouds A. Clouds are simply fogs high up in the air! 1. Clouds that form in flat sheets are stratiform clouds. 2. Vertical clouds are cumuliform clouds.

  21. B. Some of the water in a cloud can be below 0C and still exist as a liquid. This is supercooled water. http://www.howstuffworks.com/cloud.htm

  22. C. Types of clouds: (Check out chart on p. 507!) 1. Cirrus - thin, feathery, high clouds made of ice crystals

  23. 2. Stratus - low sheets or layers of clouds

  24. 3. Cumulus - puffy, cotton ball-like clouds; form from rising air. “Fair weather clouds”

  25. 4. Cirrostratus - High, thin sheets of ice clouds

  26. 5. Stratocumulus - layers of round puffs

  27. 6. Cirrocumulus - High, puffy clouds

  28. 7. Altocumulus - Higher stratocumulus clouds

  29. 8. Nimbostratus - High sheets of gray clouds that make steady rains.

  30. D. When a large mass of warm, moist air rises quickly, immense cumulonimbus clouds develop. These clouds are the basis for severe weather such as thunderstorms and tornadoes.

  31. IV. Precipitation A. How raindrops form: 1. Clouds are made up of countless microscopic water droplets 2. As air inside the cloud moves around, these droplets collide

  32. 3. Some stick together and get larger 4. When about 1,000,000 clouds droplets stick together, a rain drop forms and falls from the cloud.

  33. Forms of precipitation: • 1. Drizzle - fine droplets that fall slowly • 2. Rain - large droplets up to .25 cm diameter

  34. 3. Snow - 6-sided crystals of ice 4. Sleet - rain drops that freeze as they fall through a layer of very cold air.

  35. 5. Hail - A many-layered ice crystal that forms in enormous convection currents within a cumulonimbus cloud.

  36. C. Where does it rain? 1. Windward sides of mountain ranges. The leeward (downwind) side is usually very dry with deserts.

  37. Seattle

  38. 2. Storm areas (hurricanes, fronts, low-pressure areas, etc.) 3. Areas where global winds converge (see Reference Tables)

  39. Acid Rain - pollutants dissolve in rainwater to make it acidic. • - Affects wildlife, plants, humans, automobiles, etc.

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