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Climates of the Earth Ch. 3: Climates of the Earth
Lesson 1: Earth-Sun Relationships Lesson 2: Factors Affecting Climate Lesson 3: World Climate Patterns
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OBJECTIVE: Students will learn about the climates of the earth and how they impact humans
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Earth and Space Vocabulary
Galaxies: large groups of stars such as the Milky way. Solar system: The Sun and the group of bodies that revolve around it.
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Rotation: one complete spin of the earth on its axis.
Revolution: One elliptical orbit, every 365 ¼ days, around the sun.
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Rotation vs Revolution
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Earth-Sun Relationships
TROPICS: Warm low-latitude areas near the equator—receive solar energy all year POLAR REGIONS: areas that surround the North and South Poles—receive very little solar energy and are cold most of the time.—high latitude. MID-Latitude: solar energy changes greatly during the year.
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SEASONS Summer and Winter Solstices, June 21/December 22—the days when the sun appears directly overhead at the tropics of Capricorn/Cancer Spring and Fall Equinoxes, March 21/September 23—the days when the sun appears directly overhead at the Equator= equal days and nights.
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Climate and Weather Two main factors of both Climate and Weather:
Temperature and Precipitation
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Vocabulary Weather: condition of the atmosphere at a given time and place (DAILY). Climate: Weather conditions in a geographic region over a long time.
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Temperature: the measurement of heat
Greenhouse effect: Earth’s atmosphere traps heat energy
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Global warming: evidence that shows that Earth has gotten warmer in recent decades.
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Precipitation Precipitation: water droplets that fall in the form of rain, sleet, snow, and hail. Humidity: the amount of water vapor in the air.
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Evaporation: water changes from a liquid to a gas.
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Condensation: water vapor changes from a gas into liquid droplets.
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Elevation and Mountain Effects
An increase in elevation causes a drop in temperature. (why we have snow on mountain tops) Windward side: receives a great deal of moisture due to wind. Leeward side: as air moves down the leeward side, it warms and dries. This drier area is called a rain shadow.
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Orographic effect: when air pushes against a mountain, the mountains force the air to rise. The rising air cools and condenses, forming clouds and precipitation.
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Storms Hurricanes: most powerful and destructive tropical cyclones. Heavy rain and winds higher than 155 mph. Found in the Atlantic. Typhoons: hurricanes in the Pacific. Cyclones: hurricanes in the southern hemisphere. Tornadoes: funnel clouds with thunder and lightning.
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Climate and Vegetation
Tundra Boreal Forest Temperate forest/ Temperate grassland/Desert Rain Forest/ Savanna/ Desert Climate and Vegetation HOT Decreasing Temperature COLD WET decreasing Moisture DRY
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Tropical Climates Tropical Humid: Along Equator; Equatorial South America, Congo Basin in Africa, Southeast Asia: Warm and Rainy year round with Rain totaling inches/year Tropical Wet and Dry Climate: Between humid tropics and deserts: tropic regions of Africa, South and Central America, South and Southeast Asia, Austrailia: Warm all year; distinct rainy and dry seasons
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Tropical Humid
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Tropical Wet and Dry
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Dry Arid: centered along 30degree latitude; less than 10 inches of rain/year Semi arid: borders deserts and interiors of large continents: about inches of rain per year hot summers and cooler winters with wide temperature ranges.
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Arid
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Semiarid
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Middle-Latitude Climates
Mediterranean: only coastal Humid Subtropical —found on eastern side of continents where there are warm ocean currents. Marine West Coast Climate —heavily influenced by oceans Humid Continental —found on interiors. Has 4 distinct seasons.
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Humid Subtropical
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Mediterranean
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Marine West Coast
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Humid Continental
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High Latitude and Highland Climates
Subarctic Climate: above 50 degrees north latitude Tundra Climate: coastal areas in high latitudes/permafrost—permanently frozen soil Ice Cap Climate: Polar regions Highland Climate: Varying climates changes with elevation
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Subarctic
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Tundra
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Ice Cap
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Highlands
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