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End Show Slide 1 of 26 Copyright Pearson Prentice Hall 4-1 The Role of Climate.

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1 End Show Slide 1 of 26 Copyright Pearson Prentice Hall 4-1 The Role of Climate

2 End Show 4-1 The Role of Climate Slide 2 of 26 Copyright Pearson Prentice Hall What Is Climate? Weather is the day-to-day condition of Earth's atmosphere at a particular time and place. Climate refers to the average year-after-year conditions of temperature and precipitation in a particular region.

3 End Show 4-1 The Role of Climate Slide 3 of 26 Copyright Pearson Prentice Hall

4 End Show 4-1 The Role of Climate Slide 4 of 26 US Climate Copyright Pearson Prentice Hall

5 End Show 4-1 The Role of Climate Slide 5 of 26 Copyright Pearson Prentice Hall What Is Climate? Climate is caused by: trapping of heat by the atmosphere latitude transport of heat by winds and ocean currents amount of precipitation shape and elevation of landmasses

6 End Show 4-1 The Role of Climate Slide 6 of 26 Copyright Pearson Prentice Hall The Greenhouse Effect How does the greenhouse effect maintain the biosphere's temperature range?

7 End Show 4-1 The Role of Climate Slide 7 of 26 Copyright Pearson Prentice Hall The Greenhouse Effect Atmospheric gases that trap the heat energy of sunlight and maintain Earth's temperature range include: carbon dioxide (CO 2 ) Methane (CH 4 ) water vapor (H 2 O)

8 End Show 4-1 The Role of Climate Slide 8 of 26 Copyright Pearson Prentice Hall The Greenhouse Effect The natural situation in which heat is retained in Earth’s atmosphere by this layer of gases is called the greenhouse effect. Sunlight Earth’s Surface Atmosphere Some heat escapes into space Greenhouse gases trap some heat

9 End Show 4-1 The Role of Climate Slide 9 of 26 Copyright Pearson Prentice Hall The Effect of Latitude on Climate Solar radiation strikes different parts of Earth’s surface at an angle that varies throughout the year. At the equator, energy from the sun strikes Earth almost directly. At the North and South Poles, the sun’s rays strike Earth’s surface at a lower angle.

10 End Show 4-1 The Role of Climate Slide 10 of 26 Copyright Pearson Prentice Hall The Effect of Latitude on Climate As a result of differences in latitude and thus the angle of heating, Earth has three main climate zones: polar temperate tropical

11 End Show 4-1 The Role of Climate Slide 11 of 26 Copyright Pearson Prentice Hall The Effect of Latitude on Climate Earth’s Main Climate Zones Sunlight Most direct sunlight 90°N North Pole Temperate Tropical Temperate Polar Arctic Circle Tropic of Cancer Equator Tropic of Capricorn Antarctic Circle 90°S South Pole 66.5°S 23.5°S 23.5°N 66.5°N Polar Sunlight 0°

12 End Show 4-1 The Role of Climate Slide 12 of 26 Seasons Copyright Pearson Prentice Hall

13 End Show 4-1 The Role of Climate Slide 13 of 26 Copyright Pearson Prentice Hall Heat Transport in the Biosphere Unequal heating of Earth’s surface drives winds and ocean currents, which transport heat throughout the biosphere.

14 End Show 4-1 The Role of Climate Slide 14 of 26 Copyright Pearson Prentice Hall Heat Transport in the Biosphere Earth’s Winds WINDS 66.5°N N 23.5°N 0° 23.5°S 66.5°S Prevailing winds Southeast Trade Winds Westerlies Polar Easterlies Equator Northeast Trade Winds Westerlies Polar Easterlies

15 End Show 4-1 The Role of Climate Slide 15 of 26 Copyright Pearson Prentice Hall Heat Transport in the Biosphere Surface ocean currents warm or cool the air above them, affecting the weather and climate of nearby landmasses. OCEAN CURRENTS 66.5°N N 23.5°N 00°00° 23.5 23.5°S 66.5°S Equator Warm currents Cold currents

16 End Show - or - Continue to: Click to Launch: Slide 16 of 26 Copyright Pearson Prentice Hall 4-1

17 End Show Slide 17 of 26 Copyright Pearson Prentice Hall 4-1 The Earth’s polar zones are cold because a.they are never heated by the sun. b.at the poles, the sun's rays are at a very low angle. c.the greenhouse effect does not occur at the poles. d.heat is transported from the poles to the equator.

18 End Show Slide 18 of 26 Copyright Pearson Prentice Hall 4-1 The upward movement of warm air and the downward movement of cool air creates a.upwellings. b.air currents. c.ocean currents. d.the greenhouse effect.

19 End Show Slide 19 of 26 Copyright Pearson Prentice Hall 4-1 Earth's temperature range is maintained by a.the greenhouse effect. b.climate zones. c.ocean currents and winds. d.latitude differences.

20 End Show Slide 20 of 26 Copyright Pearson Prentice Hall 4-1 Variation of temperature in the temperate zone is due primarily to a.air and ocean currents. b.the greenhouse effect. c.variation in the sun’s energy production. d.latitude and season.

21 End Show Slide 21 of 26 Copyright Pearson Prentice Hall 4-1 The tropical zone is warm all year long because a.the sun’s angle changes the most in that part of Earth. b.ocean water is warmest near the equator. c.it receives direct or nearly direct sunlight year-round. d.landmasses in the tropic latitudes hold on to heat.

22 END OF SECTION


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