Chapter 58: The Biosphere - Effects of Sun, Wind, Water o Biosphere: includes all living communities on earth o Influences of global patterns of life Solar radiation reaching different areas Global atmospheric circulation influences oceanic circulation Some parts of earth’s surface receive more energy from the sun than others Angle of incidence: how the Sun’s rays strike the spherical Earth Earth’s rotations affect climate - Seasons Global circulation patterns - Heating at equator causes air to rise from surface to atmosphere - Radiation at the equator provides heat for water evaporation - Warm air moves north and south - cooler air flows towards equator - air descends at 30 degrees latitude (desert regions)- 60 degrees air rises again o The Coriolis Effect: curvature of the paths of the wind due to Earth’s rotation Northern hemisphere: winds curve to the right Southern hemisphere: winds curve to the left; blow westward and towards the equator Ocean currents are largely driven by winds o Regional and local differences affecting ecosystems Rain shadows- Rain falls as air rises and land remains dry on the leeward side of the mountain Monsoons: seasonally shifting winds - Asia’s size causes heating and cooling of surface causes massive regional shifts in wind patternso Winds blow water interior in summer o Winds blow to water in the winter o Winds affect duration and strength of rainfall patters Conditions such as temperature change with elevation - Temp falls about 6 degree Celsius for every 1000 m increase in elevationo Microclimates: highly localized sets of climatic conditions Gaps in forest canopy have high air temperature and low humidity under a log in a forest has low air temperature and high humidity - Biomes o Biome: a major type of ecosystem on land o Biomes are each defined by sets of regional climatic conditions and are named for their vegetal structures o Tropical Rain Forests 140-459 cm rain/year Richest ecosystems on land High temperature, rainfall, and diversity Ex: Amazon rain forest o Savanna 50-125 cm rain/year tropical or subtropical grasslands transitional ecosystem between rainforests and deserts ex: Serengeti o Deserts 25-40 cm rainfall/year plants and animals can’t depend on any rainfall 30 degrees N and S latitudes due to global air circulation patterns sparse vegetation, animals adapted to little water ex: Sahara o Temperate Grasslands or Prairies Rich soils Grasses with deep roots Converted to agricultural roots in NA Adapted to periodic fire Ex: Great Plains o Temperature Deciduous Forests Mild but seasonal climates and plentiful rains o Temperature Evergreen Forests Occur along coastlines with temperate climates o Taiga and Tundra Both stretch in unbroken circles around the entire globe o Freshwater Habitats 2% of Earth’s surface Life depends on oxygen availability from photosynthesis and aeration from atmosphere- Removed by animal and detritivore respiration- Warm water has less O2 than cool water Lake and pond habitats change with depth- Intensity of light decreases with depth - Photic: light penetrates and photosynthesis is possible - Littoral zone: shallows at edge of lake- Aphotic (benthic): below light penetration Thermal stratification: warm water is less dense than cold water and tends to float on top- Thermocline: a transition layer between warm and cold waters - Cuts of oxygen supply to bottom layer - Anoxia: oxygen depleted waters - Wind can mix and overturn layers Oligotrophic water: low in nutrients, usually high in oxygen - Crystal clear because of low organic matter- Light penetrates deep Eutrophic water: high in nutrients, densely populated with algae and plant material- Low in dissolve O2 in summer- Light doesn’t penetrate water column o Marine Habitats 71% earth’s surface is ocean continental shelves: near coastline, water is not very deep principle primary producers are phytoplankton average depth of open ocean is 4000-5000 m Ocean Zones - Open oceans have low primary productivity - Oligotrophic ocean low nutrient levels; biological deserts - continental shelf ecosystems provide abundant resources - neritic waters: waters over shelves with high concentrations of nitrates and other nutrients; shallow upwelling occurs o 99% open ocean food comes from neritic watero petroleum comes from shelves Estuaries: shelf ecosystems where fresh water from streams or rivers mix with ocean water -Intertidal habitat: area exposed to air at low tide but under water high tide -Salt marshes: in intertidal zones-Mangrove swamps: occur in tropical and subtropical intertidal zones Banks: local shallow areas on shelves; fishing Coral reefs occur in subtropical and tropical latitudes with stony corals -Algal symbioses: cnidarians and dinoflagellates Upwelling regions: localized places where deep water is drawn consistently to the surface El Nino Southern Oscillation (ENSO)-2-7 years on an irregular and unpredictable basis -coastline waters are profoundly warm-primary productivity low -weakening of east to west trade winds -upwelling only recirculates the thick, warm surface layer -wreaks havoc on ecosystems o plankton abundance drops, fish stocks disappear, sea birds and sea lions crash -heavy rains produce abundant seeds, land birds flourish, rodent and predator populations growDeep Sea: cold dark place with fascinating communities and no season -Food originates from photosynthesis in sunlit water-99% eaten as it drifts down -animals are small bodied and thinly distributed-hydrothermal vent communities: lots of life o large bodied animalso depend on sulfur oxidizing bacteria for primary production instead of the sun o water temp can be up to 350 degrees Celsius -Human Impacts: Pollution o DDT: insecticide sprayed in US after WWII that caused population of large birds to plummet because of biomagnification Egg shells became thin and broke during incubation o Freshwater habitats threatened by pollution and resource use o point source pollution: comes from an identifiable location ex: factories and sewage treatment plants laws and technologies can be applied because the source is known o diffuse pollution: ex: eutrophication caused by excessive runoff of nitrates and phosphatesdissolved O2 declines; fish species change; carp take
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