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Environmental Problems, Their Causes, and Sustainability 1

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Oxygenreleased byvegetationDiverseecologicalhabitatTree plantationEvapotranspiration decreasesLeaf litterimprovessoil fertilityForested HillsideTree rootsstabilize soil <strong>and</strong>aid water flowSteadyriver flowEvapotranspirationTrees reduce soilerosion from heavyrain <strong>and</strong> windVegetation releaseswater slowly <strong>and</strong>reduces floodingAgriculturall<strong>and</strong>After DeforestationRoadsdestabilizehillsidesGullies <strong>and</strong>l<strong>and</strong>slidesHeavy rain leachesnutrients from soil<strong>and</strong> erodes topsoilRanchingacceleratessoil erosion bywater <strong>and</strong> windSilt from erosion blocksrivers <strong>and</strong> reservoirs <strong>and</strong>causes flooding downstreamWinds removefragile topsoilAgricultural l<strong>and</strong>is flooded <strong>and</strong>silted upRapid runoffcauses floodingFigure 15-25 Natural capital degradation: hillside before <strong>and</strong> after deforestation. Once a hillside has beendeforested for timber <strong>and</strong> fuelwood, livestock grazing, or unsustainable farming, water from precipitationrushes down the denuded slopes, erodes precious topsoil, <strong>and</strong> floods downstream areas. A 3,000-year-oldChinese proverb says, “To protect your rivers, protect your mountains.”<strong>and</strong> unsustainable farming on steep <strong>and</strong> easily erodiblemountain slopes—have greatly diminished theability of its mountain soils to absorb water.Think of a forest as a complex living sponge forcatching, storing, using, <strong>and</strong> recycling water <strong>and</strong> releasingit in small amounts. Cut down the forests onthe Himalayan mountains <strong>and</strong> what happens? Insteadof being absorbed <strong>and</strong> released slowly, water from themonsoon rains runs off the denuded Himalayan foothills,carrying vital topsoil with it (Figure 15-25, right).This increased runoff of soil, combined with heavier-than-normalmonsoon rains, has increased theseverity of flooding along Himalayan rivers <strong>and</strong>downstream in Bangladesh. A disastrous flood in 1998covered two-thirds of Bangladesh’s l<strong>and</strong> area for 9months, leveled 2 million homes, drowned at least2,000 people, <strong>and</strong> left 30 million people homeless. Italso destroyed more than one-fourth of the country’scrops, which caused thous<strong>and</strong>s of people to die of starvation.In 2002, another flood left 5 million peoplehomeless <strong>and</strong> inundated large areas of rice fields.Living on Bangladesh’s coastal floodplain alsocarries dangers from storm surges <strong>and</strong> cyclones. In1970, as many as 1 million people drowned in onestorm, <strong>and</strong> another surge killed an estimated 139,000people in 1991.In their struggle to survive, the poor in Bangladeshhave cleared many of the country’s coastal mangroveforests for fuelwood, farming, <strong>and</strong> aquaculture pondsfor raising shrimp. This has led to more severe floodingbecause these coastal wetl<strong>and</strong>s help shelter Bangladesh’slow-lying coastal areas from storm surges <strong>and</strong>cyclones. Damages <strong>and</strong> deaths from cyclones in areasof Bangladesh still protected by mangrove forests havebeen much lower than in areas where the forests havebeen cleared.How Can We Reduce Flood Risks?Think about Where You Want to LiveWe can reduce flooding risks by controlling riverwater flows, preserving <strong>and</strong> restoring wetl<strong>and</strong>s,identifying <strong>and</strong> managing flood-prone areas, <strong>and</strong> ifpossible choosing not to live in such areas.We can use several methods to reduce the risk fromflooding. One is to straighten <strong>and</strong> deepen streams, aprocesscalled channelization (Figure 15-24, middle). Channelizationcan reduce upstream flooding but it removesbank vegetation <strong>and</strong> increases stream velocity. This increasedflow of water can promote upstream bank erosion,increase downstream flooding <strong>and</strong> sediment deposition,<strong>and</strong> reduce habitats for aquatic wildlife.Another approach is to build levees or floodwallsalong the sides of streams (Figure 15-24, middle). Leveescontain <strong>and</strong> accelerate stream flow, but this increasesthe water’s capacity for doing damage downstream.They also do not protect against unusually high<strong>and</strong> powerful floodwaters, as occurred in 1993 whentwo-thirds of the levees built along the MississippiRiver in the United States were damaged or destroyed.Building dams can also reduce the threat of floodingby storing water in a reservoir <strong>and</strong> releasing it328 CHAPTER 15 Water Resources

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