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Chapter 3: Climates of the Earth
Section 1: Earth-Sun Relationships
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Seasons Earth is tilted at a 23.5° angle relative to the sun
Areas of Earth get more, less direct sun at different times of year The seasons are related to the earth’s tilt and revolution
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Solstice Marks beginning of summer and winter
Sun’s rays directly overhead at noon at furthest points north and south
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Equinox Marks the beginning of spring and autumn
Day and night are equal in length
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Weather and Climate Weather—atmospheric conditions at a particular location and time Climate—weather conditions at one location over a long period
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What Causes the Weather?
Sun: amount of solar energy received Water vapor: determines whether there will be precipitation (water droplets falling as rain, snow, sleet, or hail) Cloud cover: clouds may hold water vapor
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Precipitation Warm air rises, cools, and loses ability to hold water vapor Water vapor condenses into droplets Water droplets form clouds Heavy clouds release droplets as rain or snow
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Rain Shadow A rain shadow is the land on leeward side of hills or mountains Very little precipitation in rain shadow
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Hurricanes Huge storms that form over warm, tropical ocean waters
Hit land with heavy rain, high winds, and storm surge Called typhoons in Asia
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Tornado A powerful, funnel-shaped column of spiraling air
Born from strong thunderstorms Capable of immense damage
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Blizzards Heavy snowstorm with strong winds and reduced visibility
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Droughts Long period of time with either no or minimal rainfall
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Floods Water spreads out over normally dry land
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Section 2: Factors Affecting Climate
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Factors Affecting Climate
Wind currents Zones of latitude (closer to the poles is colder and closer to the equator is hotter) Elevation (the further above sea level the colder it is) Topography
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Changes in Climate El Niño—winds push warm Pacific Ocean waters toward the Americas La Niña—winds push warm waters toward Australia and Asia
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Global Warming Gradual warming of the earth’s atmosphere
Greenhouse effect—the earth warms due to trapped solar energy
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Section 3: World Climate Patterns
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Climate Regions Temperature and precipitation define climate regions.
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Types of Climates Tropical Wet Always hot
Daily rainfall adds up to more than 80” annually
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Tropical Wet and Dry Warm, wet summer season Cooler, dry winter season
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Semiarid Hot summers Mild to cold winters Little precipitation
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Desert Can be hot or cold Less than 10” rain per year
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Mediterranean Summers dry and hot Winters cool and rainy
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Marine West Coast Moderate temperatures
Frequently cloudy, foggy and damp
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Humid Subtropical Long periods of summer heat and humidity
Winters mild to cool
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Humid Continental Great variety of temperature and precipitation
Four distinct seasons
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Subarctic Summers are short and cool Winters are long and very cold
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Tundra Flat, treeless ring of lands around the Arctic Ocean
Very little precipitation Permafrost is the constantly frozen subsoil found in this region
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Ice Cap Snow and ice Permanently freezing temperatures
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Highlands Climate varies with latitude, elevation, topography, and location
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Section 4: Soils and Vegetation
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Soil Regions Soil is a thin layer of weathered rock, humus, air, and water Topsoil refers to the top 6” of soil Soil characteristics vary with climate
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Vegetation Regions Ecosystem—interdependent community of plants and animals Biome—the ecosystem of a region Biomes are further divided into: forest grassland desert tundra
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