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Earth and Atmosphere Review Chapter 6 - Weather and Climate Chapter 16 - Environmental Geology Chapter 14 – Food and Soil Resources
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The Atmosphere Troposphere Stratosphere 78% N, 21% O Ozone layer Fig. 20-2 p. 434
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Weather 6-1 Weather: A Brief Introduction A. Weather is short-term atmospheric conditions in an area. It is typically considered in hours or days. B. Much weather activity is due to interactions between leading edges or fronts of moving masses of warm or cold air. 1. A warm front is the boundary between a warm mass of air and the cooler air it replaces. It often results in cloudy, rainy days.
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Weather 2.A cold front is an advancing mass of cold air that stays close to the ground. It is often associated with thunderstorms and high winds. Cooler, clear weather is the result. 3.Jet streams are near the top of the troposphere and circle the Earth. They have a strong influence on weather patterns.
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Figure 6-2 Page 102 Cool air mass Warm air mass Cool air mass Anvil top Warm air mass
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Climate Temperature Precipitation Uneven heating Seasons Earth’s rotation Properties of air and water Fig. 6-5 p. 105
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Seasons Fig. 6-7 p. 106
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Air Circulation Fig. 6-10, p. 107 Fig. 6-8, p. 107
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Polar (ice) Subarctic (snow) Cool temperate Warm temperate Dry Tropical Highland Major upwelling zones Warm ocean current Cold ocean current River
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Dry woodlands and shrublands (chaparral) Temperate grassland Temperate deciduous forest Boreal forest (taiga), evergreen coniferous forest (e.g., montane coniferous forest) Arctic tundra (polar grasslands) Tropical savanna, thorn forest Tropical scrub forest Tropical deciduous forest Tropical rain forest, tropical evergreen forest Desert Ice Mountains (complex zonation) Semidesert, arid grassland Tropic of Capricorn Equator Tropic of Cancer
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Temperate grassland (Lawrence, Kansas)
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Soil Profiles in Different Biomes Fig. 4-27, p. 75
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The Earth’s Life-Support Systems Troposphere Stratosphere Hydrosphere Lithosphere Biosphere Fig. 4-7 p. 60
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Figure 16-3 Page 334 Tectonic plate Collision between two continents Oceanic tectonic plate Spreading center Oceanic tectonic plate Ocean trench Plate movement Continental crust Subduction zone Oceanic crust Oceanic crust Continental crust Mantle Inner core Hot outer core Two plates move towards each other. One is subducted back into the mantle on falling convection current. Mantle convection cell Hot material rising through the mantle Material cools as it reaches the outer mantle Cold dense material falls back through mantle
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EURASIAN PLATE CHINA SUBPLATE PHILIPPINE PLATE INDIAN-AUSTRLIAN PLATE PACIFIC PLATE JUAN DE FUCA PLATE COCOS PLATE CARIBBEAN PLATE NORTH AMERICAN PLATE SOUTH AMERICAN PLATE EURASIAN PLATE ANATOLIAN PLATE ARABIAN PLATE AFRICAN PLATE SOMALIAN SUBPLATE Carlsberg Ridge Southwest Indian Ocean Ridge ANTARCTIC PLATE Transform fault East Pacific Rise Transform fault Mid- Indian Ocean Ridge Southeast Indian Ocean Ridge Mid- Atlantic Ocean Ridge Reykjanes Ridge Transform fault Divergent ( ) and transform fault ( ) boundaries Convergent plate boundaries Plate motion at convergent plate boundaries Plate motion at divergent plate boundaries Figure 16-4 Page 335
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Lithosphere Asthenosphere Oceanic ridge at a divergent plate boundary Figure 16-5a Page 336
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Lithosphere TrenchVolcanic island arc Asthenosphere Rising magma Subduction zone Trench and volcanic island arc at a convergent plate boundary Figure 16-5b Page 336
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Igneous Rock Granite, pumice, basalt Metamorphic Rock Slate, marble, quartzite Magma (molten rock) Heat, pressure, stress Heat, pressure Melting Sedimentary Rock Shale, sandstone, limestone Deposition Transportation Erosion Weathering Figure 16-9 Page 339
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Areas of serious concern Areas of some concern Stable or nonvegetative areas Global Soil Erosion Fig. 14-7 p. 280
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Soil Erosion in the US Dust Bowl – 1930s: Fig. 14-5 p. 281 Reductions in erosion since 1987 1985 Food Security Act Dust Bowl – 1930s: Fig. 14-5 p. 281 Reductions in erosion since 1987 1985 Food Security Act
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World Desertification Fig. 14-9 p. 282
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Causes of Desertification Overgrazing Deforestation Erosion Salinization Soil Compaction Natural Climate Change Overgrazing Deforestation Erosion Salinization Soil Compaction Natural Climate Change Refer to Fig. 14-10 p. 283
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Solutions: Soil Conservation Conventional-tillage Conservation tillage Terracing Windbreaks Land Classification Refer to Fig. 14-14 p. 285 Contour farming Strip and alley cropping
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