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Environmental Problems, Their Causes, and Sustainability 1

Environmental Problems, Their Causes, and Sustainability 1

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WesterliesNortheast tradesCold deserts 60°NForests30°NHot desertsForests0°EquatorCold,dry airfallsPolar capCell 3 NorthArctic tundraEvergreen60° coniferous forestTemperate deciduousforest <strong>and</strong> grassl<strong>and</strong>Desert30°Moist air rises — rainCell 2 NorthCool, dryair fallsCell 1 NorthSoutheast tradesWesterliesForestsCold desertsHot deserts60°S30°SFigure 6-8 The earth’s rotation deflects the movement of the airover different parts of the earth <strong>and</strong> creates global patterns ofprevailing winds.0°30°60°Polar capTropical deciduous forestEquatorDesertTemperate deciduousforest <strong>and</strong> grassl<strong>and</strong>Tropicalrain forestTropical deciduous forestCool, dryair fallsCell 2 SouthMoistair rises,cools, <strong>and</strong>releasesmoistureas rainCell 1 SouthCold,dry airfallsCell 3 SouthMoist air rises — rainLOWPRESSURECool, dryairFalls, is compressed, warmsHeat releasedradiates to spaceHIGHPRESSURECondensation<strong>and</strong>precipitationRises, exp<strong>and</strong>s, coolsFigure 6-10 Natural capital: global air circulation <strong>and</strong> biomes.Heat <strong>and</strong> moisture are distributed over the earth’s surface byvertical currents that form six large convection cells (Hadleycells) at different latitudes. The direction of airflow <strong>and</strong> the ascent<strong>and</strong> descent of air masses in these convection cells determinethe earth’s general climatic zones. The resulting unevendistribution of heat <strong>and</strong> moisture over the planet’s surface leadsto the forests, grassl<strong>and</strong>s, <strong>and</strong> deserts that make up the earth’sbiomes.Warm,dry airHIGHPRESSUREFlows toward low pressure,picks up moisture <strong>and</strong> heatMoist surface warmed by sunHot, wetairLOWPRESSUREFigure 6-9 Transfer of energy by convection in the atmosphere.Convection occurs when matter warms, becomes less dense,<strong>and</strong> rises within its surroundings. This efficient means of heattransfer occurs in the planet’s interior, oceans, <strong>and</strong> atmosphere(as shown here). Distribution of heat <strong>and</strong> water occurs in the atmospherebecause vertical convection currents stir up air in thetroposphere <strong>and</strong> transport heat <strong>and</strong> water from one area to anotherin circular convection cells called Hadley cells.How Do Ocean Currents <strong>and</strong> WindsAffect Regional Climates? Moving Heat <strong>and</strong>Air AroundOcean currents <strong>and</strong> winds influence climate byredistributing heat received from the sun from oneplace to another.The oceans absorb heat from the air circulation patternsjust described, with the bulk of this heat absorbednear the warm tropical areas. This heat plusdifferences in water density create warm <strong>and</strong> coldocean currents (Figure 6-6). These currents, driven bywinds <strong>and</strong> the earth’s rotation, redistribute heat receivedfrom the sun from one place to another <strong>and</strong>thus influence climate <strong>and</strong> vegetation, especially nearcoastal areas. They also help mix ocean waters <strong>and</strong> distributenutrients <strong>and</strong> dissolved oxygen needed byaquatic organisms.http://biology.brookscole.com/miller14107

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