1. LIVING IN THE ENVIRONMENT 17 TH MILLER/SPOOLMAN Chapter 7 Climate and Biodiversity

2. Core Case Study: Different Climates Support Different Life Forms Climate -- long-term temperature and precipitation patterns – determines which plants and animals can live where Tropical: equator, intense sunlight Polar: poles, little sunlight Temperate: in-between tropical and polar

3. Three Major Climate Zones Fig. 7-1, p. 147

4. 7-1 What Factors Influence Climate? Concept 7-1 Key factors that determine an area’s climate are incoming solar energy, the earth’s rotation, global patterns of air and water movement, gases in the atmosphere, and the earth’s surface features.

5. The Earth Has Many Different Climates (1) Weather Temperature, precipitation, wind speed, cloud cover Hours to days Climate Area’s general pattern of atmospheric conditions over decades and longer

6. Fig. 7-2, p. 149 Natural Capital: Generalized Map of the Earth’s Current Climate Zones

7. Fig. 7-2, p. 149 Polar (ice)Subarctic (snow)Cool temperateHighlandWarm ocean currentRiver Warm temperateDryTropicalMajor upwelling zonesCold ocean current Arctic Circle Tropic of Cancer Tropic of Capricorn Antarctic Circle

8. The Earth Has Many Different Climates (2) Air circulation in lower atmosphere due to 1.Uneven heating of the earth’s surface by sun 2.Rotation of the earth on its axis 3.Properties of air, water, and land Ocean currents Prevailing winds Earth’s rotation Redistribution of heat from the sun Surface currents and deep currents

9. Fig. 7-3, p. 149 Global Air Circulation

10. Fig. 7-3, p. 149 Moist air rises, cools, and releases moisture as rain Cold deserts 60°N Evergreen coniferous forest The highest solar energy input is at the equator. Hot desert Northeast trades 30°N Temperate deciduous forest and grassland Temperate deciduous forest and grassland Westerlies Air cools and descends at lower latitudes. Tropical deciduous forest Warm air rises and moves toward the poles. Solar energy Equator 0° Tropical rain forest Tropical deciduous forest Southeast trades Hot desert 30°S Westerlies 60°S Cold deserts Temperate deciduous forest and grassland Air cools and descends at lower latitudes. Polar cap

11. Fig. 7-4, p. 150 Cool, dry air Condensation and precipitation Heat released radiates to space LOW PRESSUREHIGH PRESSURE Falls, is compressed, warms Rises, expands, cools Warm, dry air Hot, wet air Flows toward low pressure, picks up moisture and heat HIGH PRESSURE Moist surface warmed by sun LOW PRESSURE

12. Fig. 7-4, p. 150 Energy Transfer by Convection in the Atmosphere

13. Fig. 7-5, p. 150 Connected Deep and Shallow Ocean Currents

14. Fig. 7-5, p. 150 Warm, less salty, shallow current Cold, salty, deep current

15. The Earth Has Many Different Climates (3) El Niño-Southern Oscillation Every few years Prevailing winds in tropical Pacific Ocean change direction Affects much of earth’s weather for 1-2 years Link between air circulation, ocean currents, and biomes

16. Figure 4, Supplement 7 Normal and El Niño Conditions

17. Figure 5, Supplement 7 Impact of El Nino-Southern Oscillation

18. Greenhouse Gases Warm the Lower Atmosphere Greenhouse gases H 2 O CO 2 CH 4 N 2 O Natural greenhouse effect Gases keep earth habitable Human-enhanced global warming

19. Fig. 3-4, p. 57 Flow of Energy to and from the Earth

20. Earth’s Surface Features Affect Local Climates Differential heat absorption by land and water Land and sea breezes Rain shadow effect Most precipitation falls on the windward side of mountain ranges Deserts leeward Cities create microclimates

21. Fig. 7-6, p. 152 Rain Shadow Effect

22. Fig. 7-6, p. 152 Prevailing winds pick up moisture from an ocean. On the windward side of a mountain range, air rises, cools, and releases moisture. On the leeward side of the mountain range, air descends, warms, and releases little moisture, causing rain shadow effect.

23. 7-2 How Does Climate Affect the Nature and Locations of Biomes? Concept 7-2 Differences in average annual precipitation and temperature lead to the formation of tropical, temperate, and cold deserts, grasslands, and forests, and largely determine their locations.

24. Climate Helps Determine Where Organisms Can Live Major biomes: large land regions with certain types of climate and dominant plant life Not uniform Mosaic of patches Influenced by: Latitude and elevation Annual precipitation Temperature

25. Fig. 7-7, p. 153 The Earth’s Major Biomes

26. Figure 3, Supplement 8 North America Biomes

27. Fig. 7-8, p. 153 Generalized Effects of Elevation and Latitude on Climate and Biomes

28. Fig. 7-8, p. 153 Elevation Mountain ice and snow Tundra (herbs, lichens, mosses) Coniferous Forest Deciduous Forest Latitude (south to north) Tropical Forest Deciduous Forest Coniferous Forest Tundra (herbs, lichens, mosses) Polar ice and snow

29. Latitude Tropical Forest Deciduous Forest Coniferous Forest Tundra (herbs, lichens, mosses) Polar ice and snow Elevation Mountain ice and snow Tundra (herbs, lichens, mosses) Coniferous Forest Deciduous Forest Tropical Forest Stepped Art Fig. 7-8, p. 153

30. Fig. 7-9, p. 154 Natural Capital: Average Precipitation and Average Temperature as Limiting Factors

31. Fig. 7-9, p. 154 Cold Arctic tundra Cold desert Evergreen coniferous forest Temperate desert Temperate deciduous forest Temperate grassland Chaparral Hot Wet Tropical rain forest Dry Tropical desert Tropical grassland (savanna)

32. Figure 6, Supplement 8 Global Plant Biodiversity

33. Fig. 7-7, p. 153 Tropic of Cancer High mountains Equator Polar ice Arctic tundra (cold grassland) Temperate grassland Tropic of Capricorn Tropical grassland (savanna) Chaparral Coniferous forest Temperate deciduous forest Temperate rain forest Tropical rain forest Tropical dry forest Desert

34. There Are Three Major Types of Deserts 1.Tropical deserts 2.Temperate deserts 3.Cold deserts Fragile ecosystem Slow plant growth Low species diversity Slow nutrient recycling Lack of water

35. Fig. 7-10, p. 155 Climate Graphs of Three Types of Deserts

36. Stepped Art Fig. 7-10, p. 155

37. Figure 1, Supplement 6 Temperate Desert Ecosystem in North America

38. Science Focus: Staying Alive in the Desert Beat the heat/every drop of water counts Plant adaptations Succulents Deep tap roots Animal strategies and adaptations Physiology and anatomy Behavior

39. Fig. 7-A, p. 156 Wildflowers Bloom after Rain in Arizona

40. There Are Three Major Types of Grasslands (1) 1.Tropical 2.Temperate 3.Cold (arctic tundra)

41. Fig. 7-11, p. 157 Climate Graphs of Tropical, Temperate, and Cold Grasslands

42. Stepped Art Fig. 7-11, p. 157

43. There Are Three Major Types of Grasslands (2) Tropical Savanna Grazing animals Browsing animals Temperate Cold winters and hot and dry summers Tall-grass prairies Short-grass prairies Often converted to farmland

44. Figure 2, Supplement 6 Temperate Tall-Grass Prairie Ecosystem in North America

45. There Are Three Major Types of Grasslands (3) Arctic tundra: fragile biome Plants close to ground to conserve heat Most growth in short summer Animals have thick fur Permafrost Underground soil that stays frozen Alpine tundra: above tree line in mountains

46. Fig. 7-12, p. 158 Monoculture Crop Replacing Biologically Diverse Temperate Grassland

47. Temperate Shrubland: Nice Climate, Risky Place to Live Chaparral Near the sea: nice climate Prone to fires in the dry season

48. There Are Three Major Types of Forests (1) 1.Tropical 2.Temperate 3.Cold Northern coniferous and boreal

49. Fig. 7-13, p. 160 Climate Graphs of Tropical, Temperate, and Cold Forests

50. Stepped Art Fig. 7-13, p. 160

51. There Are Three Major Types of Forests (2) Tropical rain forests Temperature and moisture Stratification of specialized plant and animal niches Little wind: significance Rapid recycling of scarce soil nutrients Impact of human activities

52. Fig. 7-14, p. 161 Tropical Rain Forest Ecosystem

53. Fig. 7-14, p. 161 Blue and gold macaw Harpy eagle Ocelot Squirrel monkeys Climbing monstera palm Katydid Slaty-tailed trogon Green tree snake Tree frog Snail Ants Bacteria Bromeliad Fungi Producer to primary consumer Primary to secondary consumer Secondary to higher-level consumer All producers and consumers to decomposers

54. Fig. 7-15, p. 162 Niche Stratification in a Tropical Rain Forest

55. Fig. 7-15, p. 162 45 Harpy eagle Emergent layer 40 35 Toco toucan 30 Canopy 25 Height (meters) 20 Wooly opossum Understory 15 10 Brazilian tapir Shrub layer 5 Black-crowned antpitta Ground layer 0

56. There Are Three Major Types of Forests (3) Temperate deciduous forests Temperature and moisture Broad-leaf trees Slow rate of decomposition: significance Impact of human activities

57. Figure 4, Supplement 6 Temperate Deciduous Forest Ecosystem in North America

58. There Are Three Major Types of Forests (4) Evergreen coniferous forests: boreal and taigas Temperature and moisture Few species of cone: bearing trees Slow decomposition: significance Coastal coniferous forest Temperate rain forests

59. Figure 5, Supplement 6 Evergreen Coniferous Forest Ecosystem in North America

60. Fig. 7-16, p. 163 Temperate Rain Forest in Washington State

61. Mountains Play Important Ecological Roles Majority of the world’s forests Islands of biodiversity Habitats for endemic species Help regulate the earth’s climate Major storehouses of water Role in hydrologic cycle

62. Fig. 7-17, p. 163 Mount Rainier National Park in Washington State

63. 7-3 How Have We Affected the Word’s Terrestrial Ecosystems? Concept 7-3 In many areas, human activities are impairing ecological and economic services provided by the earth’s deserts, grasslands, forests, and mountains.

64. Humans Have Disturbed Most of the Earth’s Lands Deserts Grasslands Forests Mountains

65. Fig. 7-18, p. 165 Major Human Impacts on Terrestrial Ecosystems

66. Fig. 7-18, p. 165 Natural Capital Degradation Major Human Impacts on Terrestrial Ecosystems DesertsGrasslandsForestsMountains Large desert citiesConversion to cropland Clearing for agriculture, livestock grazing, timber, and urban development Agriculture Destruction of soil and underground habitat by off-road vehicles Timber and mineral extraction Release of CO 2 to atmosphere from burning grassland Conversion of diverse forests to tree plantations Hydroelectric dams and reservoirs Soil salinization from irrigation Increasing tourism Overgrazing by livestock Depletion of groundwater Damage from off- road vehicles Air pollution blowing in from urban areas and power plants Oil production and off-road vehicles in arctic tundra Soil damage from off-road vehicles Land disturbance and pollution from mineral extraction Pollution of forest streams Water supplies threatened by glacial melting

67. Mountains Agriculture Timber extraction Hydroelectric dams and reservoirs Mineral extraction Increasing tourism Urban air pollution Increased ultraviolet radiation from ozone depletion Soil damage from off-road vehicles Forests Clearing for agriculture, livestock grazing, timber, and urban development Conversion of diverse forests to tree plantations Damage from off- road vehicles Pollution of forest streams Large desert cities Soil destruction by off-road vehicles Deserts Soil salinization from irrigation Depletion of groundwater Land disturbance and pollution from mineral extraction Grasslands Conversion to cropland Release of CO 2 to atmosphere from burning grassland Overgrazing by livestock Oil production and off-road vehicles in arctic tundra Stepped Art NATURAL CAPITAL DEGRADATION Major Human Impacts on Terrestrial Ecosystems Fig. 7-18, p. 165

68. Three Big Ideas 1.Differences in climate, based mostly on long-term differences in average temperature and precipitation, largely determine the types and locations of the earth’s deserts, grasslands, and forests. 2.The earth’s terrestrial systems provide important ecological and economic services.

69. Three Big Ideas 3.Human activities are degrading and disrupting many of the ecological and economic services provided by the earth’s terrestrial ecosystems.