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Chapter 4 Moisture and Atmospheric Stability The Atmosphere 10e

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Presentation on theme: "Chapter 4 Moisture and Atmospheric Stability The Atmosphere 10e"— Presentation transcript:

1 Chapter 4 Moisture and Atmospheric Stability The Atmosphere 10e
Lutgens & Tarbuck Power Point by Michael C. LoPresto

2 Steam Fog over a Lake

3 The Hydrologic Cycle

4 Water’s Changes of State

5 Ice

6 Water

7 Condensation of Water Vapor
Generates Fog

8 Frost on a Window Pane

9 Humidity Is the Content of Water Vapor in the Air

10 Relationship between Vapor Pressure and Saturation

11 Saturation Vapor Pressure Varies with Temperature

12 Hot desert air with low relative humidity will actually have a higher water vapor-content than frigid air with high

13 Relative Humidity Changes with Added Moisture

14 Relative Humidity Changes with Temperature

15 Daily Changes in Relative Humidity with Temperature

16 Cold Drinking-glasses Chill Surrounding Air to the Dew-Point Condensation on Cold Drinking-glasses

17

18 Dew Point Temperatures

19

20 Sling Psychrometer

21 Adiabatic Temperature Changes

22 Dry and Wet Adiabatic Rates

23 Lifting Processes Orographic

24 Heavy Precipitation in Mountains
Snow Pack in the Rocky Mountains

25 Death Valley Rain Shadow Desert

26 Frontal Wedging

27 Convergence

28 Convergence over Southern Florida

29 Wetter Windward Locations and Leeward Rain Shadows

30 Convection

31 As long as air in a balloon is hotter than the surrounding air, it will rise

32 Adiabatic Cooling

33 Atmospheric Stability
Absolute Stability

34 Absolute Instability

35 Conditional Stability

36 An Unstable Atmosphere

37 Chapter 4 END


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