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Environmental Problems, Their Causes, and Sustainability 1

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Figure 4-9 Solar capital: flow of energy to <strong>and</strong>from the earth.SolarradiationEnergy in = Energy outReflected byatmosphere (34%)UV radiationAbsorbedby ozoneAbsorbedby theearthVisiblelightRadiated byatmosphereas heat (66%)Lower Stratosphere(ozone layer)GreenhouseTroposphere effectHeatEarthure 4-9. About 80% of the energy that gets throughwarms the troposphere <strong>and</strong> evaporates <strong>and</strong> cycles waterthrough the biosphere. About 1% of this incomingenergy generates winds, <strong>and</strong> green plants, algae, <strong>and</strong>bacteria use less than 0.1% to fuel photosynthesis.Most of the solar radiation making it though the atmospherehits the surface of the earth <strong>and</strong> is degradedinto longer-wavelength infrared radiation. This infraredradiation interacts with so-called greenhouse gases(such as water vapor, carbon dioxide, methane, nitrousoxide, <strong>and</strong> ozone) in the troposphere. The radiationcauses these gaseous molecules to vibrate <strong>and</strong> releaseinfrared radiation with even longer wavelengths intothe troposphere. As this radiation interacts with moleculesin the air, it increases their kinetic energy, helpingwarm the troposphere <strong>and</strong> the earth’s surface. Withoutthis natural greenhouse effect, the earth would be toocold for life as we know it to exist <strong>and</strong> you would not bearound to read this book.Heat radiatedby the earthViewed from outer space, the earth resemblesan enormous jigsaw puzzle consistingof large masses of l<strong>and</strong> <strong>and</strong> vastexpanses of ocean.Biologists have classified the terrestrial(l<strong>and</strong>) portion of the biosphere intobiomes (“BY-ohms”). They are large regionssuch as forests, deserts, <strong>and</strong> grassl<strong>and</strong>scharacterized by a distinct climate<strong>and</strong> specific species (especially vegetation)adapted to it (Figure 4-10, p. 62).Scientists divide the watery parts ofthe biosphere into aquatic life zones, eachcontaining numerous ecosystems. Examples includefreshwater life zones (such as lakes <strong>and</strong> streams) <strong>and</strong>ocean or marine life zones (such as coral reefs, coastal estuaries,<strong>and</strong> the deep ocean).What Are the Major Componentsof Ecosystems? Matter, Energy, LifeEcosystems consist of nonliving (abiotic) <strong>and</strong> living(biotic) components.Two types of components make up the biosphere <strong>and</strong>its ecosystems. One type, called abiotic, consists ofnonliving components such as water, air, nutrients,<strong>and</strong> solar energy. The other type, called biotic, consistsof biological components—plants, animals, <strong>and</strong>microbes.Figures 4-11 (p. 63) <strong>and</strong> 4-12 (p. 63) are greatlysimplified diagrams of some of the biotic <strong>and</strong> abioticcomponents in a freshwater aquatic ecosystem <strong>and</strong> aterrestrial ecosystem.4-3 ECOSYSTEM COMPONENTSWhat Are Biomes <strong>and</strong> Aquatic Life Zones? Lifeon L<strong>and</strong> <strong>and</strong> at SeaLife exists on l<strong>and</strong> systems called biomes <strong>and</strong> infreshwater <strong>and</strong> ocean aquatic life zones.How Tolerant Are Organisms to<strong>Environmental</strong> Conditions? ToleranceLimitsPopulations of different species can thrive onlyunder certain physical <strong>and</strong> chemical conditions.Populations of different species thrive under differentphysical conditions. Some need bright sunlight, <strong>and</strong>http://biology.brookscole.com/miller1461

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