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Ecology and the Biosphere

Ecology and the Biosphere

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Ecology and the Biosphere

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  1. Ecology and the Biosphere Chapter 52

  2. Earth from the moon

  3. Ecology • Ecology is the study of Distribution and Abundance of organisms over time. • Distribution is where we naturally find / found an organism • Abundance is how many individuals are / were counted at the study sites

  4. Organismal ecology Fig. 52-2 Population ecology Community ecology Ecosystem ecology Landscape ecology Global ecology

  5. Ecological levels • Populations include all the members of one species in a given area and time. • Species include all of the potentially interbreeding populations. • Community includes all of the different species (plants, animals, fungi, etc.) living in the area • Ecosystem includes the Biotic and Physical components of the environment • Landscape- Interactions between connected ecosystems • Biosphere is world –wide issues, like Global warming, and pollution

  6. Climate • Determines what plants can grow there • Two major factors of climate: • Temperature (warm to cold) • Precipitation (moisture – wet to dry) • Position on globe determines climate

  7. Temperature • Simple gradient from warm to cold by increasing latitude • Solar intensity greatest and warmer at equator (0o) • Less intense and cooler at poles (90o).

  8. Solar radiation

  9. Solar radiation around the Globe Solar radiation around the Globe

  10. Precipitation • Alternating bands of wet and dry areas along a latitudinal gradient • Wet at equator 00, and 600 N / S • Dry at 300, and 900 poles • Poles are frozen deserts • Caused by formation of Hadley Cells

  11. Hadley Cells • Air rises (00, 600) due to warming of surface. • as the air rises it becomes less dense and cooler, dropping water as rain. • Air falls (300, 900 poles) • air becomes compressed, and heats. It absorbs moisture and falls as dry air.

  12. Global air circulation, precipitation, and winds: Hadley cells

  13. Convection Currents • Global air circulation is affected by the properties of air water, and land. Figure 5-5

  14. Global Air Circulation Hadley cell

  15. West Coast Latitudes • Dry : nearer 300 • San Diego=32.5; LA= 34; Sta. Barbara= 34.5 • Santa Cruz =37, SF 37.75; • Eureka= 40.75 • Wetter nearing 600: • Portland= 45.5; Seattle= 47.5 • Juneau= 58; Anchorage = 61

  16. Hadley - Ferrel cells

  17. Coriolis Effect • Global air circulation is affected by the rotation of the earth on its axis. Figure 5-4

  18. Prevailing winds • These Hadley cell wind currents move North or South • The spinning of the earth makes it seem like they come at an angle. • In CA our winds, storms usually come from the south west. • Our Rains often bring warmer weather

  19. Global Trade Wind Patterns

  20. Ocean currents • Prevailing winds cause ocean waters to move in the prevailing direction. • Northern Pacific flows clockwise • Sea level 4 feet higher in Asia • Water flows from Alaska southwards along our coast • Near shore upwelling brings cold, nutrient rich water up along our shore • Very high productivity of tidal areas

  21. Ocean Currents

  22. Upwelling Wind from the north starts surface ocean water moving c. Deep, cold water moves up to replace water moving west Earth's rotational force deflects moving water westward

  23. Seasons • Caused by tilting of earth on its rotational axis. • Intensity of sunlight varies. • Most extreme at poles • Little change at equator.

  24. Seasons- • Tilting of earth moves solar equator. • Effectively moves solar 300 dry zone north in summer • The wet belt moves farther south giving us wet winters

  25. Causes of Seasons

  26. Biomes • Major vegetation types that also determine the animal community present. • Determined mostly by climate • Soil also important factor

  27. Common California Biomes Dry to Wet • Desert - driest • Chaparral – shrubs with fire cycle • Grasslands – no trees, all grass • Savanna – widely spaced trees in grass • Woodland – open canopy • Forest – closed canopy, wettest

  28. A climograph for some major kinds of ecosystems (biomes) in North America

  29. Biomes

  30. Major Biomes

  31. Patterns of distribution in the biosphere

  32. Coniferous forest, Lady Bird Grove (top left), Sequoias (right), rain forest (bottom left)

  33. Temperate deciduous forest, Great Smokey Mountains National Park

  34. Tropical forests

  35. Savanna

  36. Desert. Organ Pipe State Park (top), Joshua Tree National Park (bottom left), Death Valley (bottom right)

  37. Temperate grassland- Prairie

  38. Tundra. Denali National Park (left), reindeer (right)

  39. Rain shadow • Precipitation increases as storms are pushed up over mountains. • accordingly rain becomes snow • As air moves up slope in the Sierras it cools 3-5 degrees per 1,000 ft. • This is the same effect as moving 300 miles farther north ! • Causes deserts in Nevada • Most islands with mountains have wet and dry sides

  40. Rainshadow

  41. Rainshadow

  42. Biotic Zonation of Sierras

  43. Summer Fog

  44. Summer Fog • Inland air warms quickly. This rising air, pulls in coastal air. • Marine air is pulled inland by this draw in the Central valley – causing summer winds over the low passes (Altamont) • Cold water off CA. coast cools incoming warm, moist ocean air- causing condensation. • Essential for ranges of Coast Redwoods, relic pines and cypress species . • Can add up to 10 inches of summer precipitation in some areas.

  45. FOG HEAVEN / The sun will come out tomorrow. Or maybe not. It's summer in the city, and that means gray skies.What causes fog. Chronicle Graphic

  46. Central Valley Smog : weblog.rudayday.com/archives/2005_08.html

  47. Smog moves up into Sierras

  48. Temperature Inversion layers • dense air flows downhill and collects in low spots, valleys. Great Central valley is an example. • This dense air may be blocked by hills etc. from warmer winds which blow over the top of dense air, leaving it alone. • Dense tule fog may form for days. • Inversion layer (cold air higher up) also traps pollutants. • Mexico City problems • Reno, Tahoe now ban fireplaces. • Often “burn off” in summer but leave the haze of phytochemical smog behind.

  49. Ocean Zones • Intertidal – species rich zone on rocks between high and low tides levels. • Photic – upper sunlit layers where phytoplankton (producers) live • Neritic – productive zone over Continental Shelf • Oceanic - Open Ocean, nutrient poor low productivity