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Chapter 6 CLIMATE, TERRESTRIAL BIODIVERSITY, & AQUATIC BIODIVERSITY.

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Presentation on theme: "Chapter 6 CLIMATE, TERRESTRIAL BIODIVERSITY, & AQUATIC BIODIVERSITY."— Presentation transcript:

1 Chapter 6 CLIMATE, TERRESTRIAL BIODIVERSITY, & AQUATIC BIODIVERSITY

2 5 factors that determine global air circulation patterns What causes it?How does it affect air circulation? 1. Uneven heating of Earth 2. Seasons 3. Earth’s rotation 4. Variation of sun’s output 5. Properties of air and water

3 1. Uneven Heating of the Earth

4 5 factors that determine global air circulation patterns What causes it?How does it affect air circulation? 1. Uneven heating of Earth 2. Seasons 3. Earth’s rotation 4. Variation of sun’s output 5. Properties of air and water

5 2. Seasons

6 5 factors that determine global air circulation patterns What causes it?How does it affect air circulation? 1. Uneven heating of Earth 2. Seasons 3. Earth’s rotation 4. Variation of sun’s output 5. Properties of air and water

7 3. Rotation of Earth

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10 5 factors that determine global air circulation patterns What causes it?How does it affect air circulation? 1. Uneven heating of Earth 2. Seasons 3. Earth’s rotation 4. Variation of sun’s output 5. Properties of air and water

11 4. Variations in solar output

12 Sun Spots

13 http://sohowww.nascom.nasa.gov/data/ realtime/gif/ http://sohowww.nascom.nasa.gov/data/ realtime/gif/

14 5 factors that determine global air circulation patterns What causes it?How does it affect air circulation? 1. Uneven heating of Earth 2. Seasons 3. Earth’s rotation 4. Variation of sun’s output 5. Properties of air and water

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16 5. Properties of air and land

17 Valley (in-land) cities

18 5. Properties of air and land Coastal cities

19 5 factors that determine global air circulation patterns What causes it?How does it affect air circulation? 1. Uneven heating of Earth 2. Seasons 3. Earth’s rotation 4. Variation of sun’s output 5. Properties of air and water

20 How do ocean currents affect regional climates?

21 28,000 rubber duckies lost at sea

22 Other items lost at sea 1992 – 80,000 Nike sneakers 1994 – 34,000 hockey gloves 1997 – 5 million LEGO pieces 2002 – 33,000 Nike sneakers

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24 Ocean Currents In which direction is the warm water flowing? How does that affect the climate?

25 Ocean Upwellings When have you experienced upwellings before?

26 Ocean Upwelling

27 El Niño is a disruption of the ocean-atmosphere system in the Tropical Pacific having important consequences for weather and climate around the globe. El Niño - “The Christ Child”

28 Normal Conditions Wind blows from east to west (right to left) Pushes water to western Pacific Causes LOTS of rain (monsoons & snow in Himalaya Mts.) Water flows along bottom & up at South America

29 The Normal Pacific

30 Normal Conditions Strong east to west winds, rain in west, cold water east coast Thermocline - boundary between cold and warm water

31 El Niño

32 Note the change in wind and ocean currents during El Niño

33 El Niño Weak east to west winds, rain in middle, warm water east coast

34 Trade winds push warm ocean water west, cool water rises behind it Trade winds ease and switch directions, warmest water moves east

35 Earth’s warmest ocean water in the far western Pacific energizes huge thunderstorms Warm water, thunderstorms move eastward Thunderstorms disrupt jet stream patterns

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37 El Niño Conditions Water warms (+1º C average) Winds weaken Upwelling stops Climate changes We do not know why this happens

38 Note the lower catch levels during El Niño

39 How does the chemical make-up of the atmosphere lead to the greenhouse effect?

40 What are greenhouse gases? Atmospheric gases that absorb infrared radiation, which warms the air Examples: –CO 2 –H2O–H2O–H2O–H2O –CH 4 –NO 2 –CFCs

41 Are greenhouse gases GOOD or BAD? THEY’RE BOTH GOOD - without greenhouse gases, the Earth would be too cold for life BAD - too many greenhouse gases may lead to global warming

42 Where do greenhouse gases come from? ALL OF US!!! Burning fossil fuels releases: –CO 2 –H2O–H2O–H2O–H2O –NO 2 Cows release methane (CH 4 ) Various refrigerants use CFCs

43 Ozone Depletion Is this what the hole in the ozone layer looks like?

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47 Ozone Videos http://www.youtube.com/watch?v=qUfVMo gIdr8 http://www.youtube.com/watch?v=qUfVMo gIdr8 http://www.youtube.com/watch?v=vuFhaa wqsNM&feature=related http://www.youtube.com/watch?v=vuFhaa wqsNM&feature=related

48 Rain Shadow Effect

49 Molokai, Hawaii wind

50 What’s the difference between a climate and a biome? Climate: physical properties (temperature and precipitation) of an area over a long period of time Biome: areas on Earth that are inhabited by certain types of organisms

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55 Desert Biomes

56 Characteristics typically < 25 cm (10 in) annual precipitation cover 30% of the world’s land surface especially found at 30° N and 30° S latitude largest deserts on interiors of continents © Brooks/Cole Publishing Company / ITP

57 30º N 30º S

58 Deserts

59 Desert Biomes Desert Organisms sparse, widely spaced, mostly low vegetation plants typically deep–rooted shrubs with small leaves, succulents, or short–lived species that flourish after rain animals typically nocturnal & have physical adaptations for conserving water & dealing with heat.

60 Grassland Biomes Figs. 6–14 © Brooks/Cole Publishing Company / ITP

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62 Grassland Biomes Characteristics sufficient rainfall to support grass, but too dry for forests mostly found on interiors of continents maintained by seasonal drought, grazing, & periodic fires that prevent shrubs & trees invasion © Brooks/Cole Publishing Company / ITP

63 Grassland Biomes Characteristics – –plants include high diversity of grasses & herbaceous plants; typically have resistance to drought, grazing, & fire – –animals include large & small herbivores, along with predators adapted to feed on these herbivores

64 Forest Biomes Fig. 6–17 © Brooks/Cole Publishing Company / ITP

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66 Forest Biomes Characteristics: sufficient rainfall to support trees types: -Tropical – typically broadleaf evergreen trees with high diversity -Temperate – typically deciduous broadleaf tree with moderate diversity -Boreal – typically conifers with low diversity © Brooks/Cole Publishing Company / ITP

67 Forest Biomes Characteristics: various layers: -Emergent – tree tops that break through the canopy -Canopy – “roof” of forest of full grown trees. -Understory – dark and composed of tree saplings -Forest Floor – dark, not crowded

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69 Precipitation TemperatureWetModerateDry Hot Temperate Cold

70 Precipitation TemperatureWetModerateDry Hot Tropical Forest Tropical Grassland Tropical Desert Temperate Temperate Forest Temperate Grassland Temperate Desert Cold Polar Forest Polar Grassland Polar Desert

71 Mountain Biomes Characteristics – –diversity of habitat because of diverse topography – –make up 20% of Earth's surface – –each 100 m (~300 ft) gain in elevation is about equal to 100 km (~62 mi) change in latitude – –mountain regions contain majority of world's forests – –timberline: elevation above which trees do not grow – –gradually release melting ice, snow, and water to streams

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73 Important Biome Concepts everything is connected incoming solar radiation determines global temperature & precipitation patterns temperature & precipitation are major determinants of distribution of organisms


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