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Chapter 5 Atmospheric Water and Weather
Elemental Geosystems 5e Robert W. Christopherson Charles E. Thomsen
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Water and Atmospheric Moisture
Water on Earth: Location and Properties Humidity Atmospheric Stability Clouds and Fog Air Masses Atmospheric Lifting Mechanisms Midlatitude Cyclonic Systems Violent Weather
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Water on Earth Quantity Equilibrium
Distribution of Earth’s Water Today Unique Properties of Water Heat Properties Ice Water Water vapor Heat properties of water in nature
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Land and Water Hemispheres
Figure 5.2
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Ocean and Freshwater Distribution
Figure 5.3
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Three States of Water Figure 5.4
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Water’s Heat Energy Characteristics
Figure 5.6
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Humidity Relative Humidity Expressions of Humidity Vapor pressure
Specific humidity Instruments for measurement
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Relative Humidity Figure 5.7
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Humidity Patterns Figure 5.10
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Maximum Specific Humidity
Figure 5.12
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Humidity Instruments Figure 5.13
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Atmospheric Stability
Adiabatic Processes Dry adiabatic rate (DAR) Moist adiabatic rate (MAR) Stable and unstable atmospheric conditions
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Buoyancy Figure 5.14
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Adiabatic Processes Figure 5.15
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Atmospheric Temperatures and Stability
Figure 5.16
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Clouds and Fog Cloud Types and Identification Fog Advection fog
Radiation fog
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Cloud Types and Identification
Figure 5.18
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Cumulonimbus Development
Figure 5.19
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Advection Fog Figure 5.20
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Evaporation Fog Figure 5.21
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Valley Fog Figure 5.25 Figure 5.22
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Radiation Fog Figure 5.23
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Air Masses Figure 5.24
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Atmospheric Lifting Mechanisms
Convectional Lifting Orographic Lifting Frontal Lifting Cold fronts Warm fronts
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Atmospheric Lifting Mechanisms
Figure 5.27
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FIGURE 7. 6 The distribution of ice and water
in a cumulonimbus cloud.
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FIGURE 7.9 The ice-crystal (Bergeron) process.
(1) The greater number of water vapor molecules around the liquid droplet causes water molecules to diffuse from the liquid droplet toward the ice crystal. (2) The ice crystal absorbs the water vapor and grows larger, while (3) the water droplet grows smaller.
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FIGURE 7. 21 An accumulation of rime forms on tree branches
as supercooled fog droplets freeze on contact in the below-freezing air.
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FIGURE 7. 22 A heavy coating of freezing rain (glaze) covers Syracuse,
New York, during January, 1998, causing tree limbs to break and power lines to sag.
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FIGURE 7. 4 Collision and coalescence. (a) In a warm cloud
composed only of small cloud droplets of uniform size, the droplets are less likely to collide as they all fall very slowly at about the same speed. Those droplets that do collide, frequently do not coalesce because of the strong surface tension that holds together each tiny droplet. (b) In a cloud composed of different size droplets, larger droplets fall faster than smaller droplets. Although some tiny droplets are swept aside, some collect on the larger droplet’s forward edge, while others (captured in the wake of the larger droplet) coalesce on the droplet’s backside.
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FIGURE 7. 28 This giant hailstone — the largest ever reported in
the United States with a diameter of 17.8 cm (7 in.) — fell on Aurora, Nebraska, during June, 2003.
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Lake Effect Snowbelts Figure 5.26
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Local Heating and Convection
Figure 5.28
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Convection over Florida
Figure 5.29
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Orographic Precipitation
Figure 5.30
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Cold Front Figure 5.31a
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Cold Front and Squall Line
Figure 5.31b
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Warm Front Figure 5.32
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Midlatitude Cyclonic Systems
Life Cycle of a Midlatitude Cyclone Storm tracks Open stage Occluded stage
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Midlatitude Cyclone Figure 5.33
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Average and Actual Storm Tracks
Figure 5.34
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Midlatitude Cyclone Figure 5.35
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Weather Forecasting Figure
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Violent Weather Thunderstorms Derechos Tornadoes Tropical Cyclones
Atmospheric turbulence Lightning and thunder Hail Derechos Tornadoes Tornado measurement and science Tropical Cyclones Hurricanes and typhoons Physical structure A final word
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Thunderstorms Figure 5.36
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Thunderstorms Figure 5.37
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Twister! Figure 5.38
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Tornadoes Figure 5.39
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Tropical Cyclones Figure 5.40
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Brazilian Hurricane Figure 5.40
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2005 Hurricane Season Figure 5.41
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Profile of a Hurricane Figure 5.42
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Elemental Geosystems 5e
End of Chapter 5 Elemental Geosystems 5e Robert W. Christopherson Charles E. Thomsen
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