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Published byNigel Gardner Modified over 8 years ago
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This lecture will help you understand: Water and the hydrologic cycle Water’s distribution on Earth Freshwater ecosystems Use and alteration of freshwater systems The marine environment
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Freshwater systems Water may seem abundant, but drinkable water is rare Freshwater = relatively pure, with few dissolved salts Only 2.5% of Earth’s water is fresh Most freshwater is tied up in glaciers and ice caps
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Water storage Water Reservoir – a place in the atmosphere, ocean or underground where water is stored for a period of time
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Rivers & streams wind through landscapes Water from rain, snowmelt, or springs forms streams, creeks or brooks These merge into rivers, and eventually reaches the ocean Tributary = a smaller river flowing into a larger one Watershed = the area of land drained by a river and its tributaries
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Rivers & streams wind through landscapes Hydrology – the study of the occurrence, distribution and movement of water on, in & above the Earth
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A river may shift course Floodplain = areas nearest to the river’s course that are flooded periodically Frequent deposition of silt makes floodplain soils fertile Riparian = riverside areas that are productive and species-rich Water of rivers and streams hosts diverse ecological communities
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Wetlands include marshes, swamps, and bogs Wetlands = systems that combine elements of freshwater and dry land Freshwater marshes = shallow water allows plants to grow above the water’s surface Swamps = shallow water that occurs in forested areas Can be created by beavers Bogs = ponds covered in thick floating mats of vegetation A stage in aquatic succession
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Wetlands are valuable Wetlands are extremely valuable for wildlife They slow runoff Reduce flooding Recharge aquifers Filter pollutants People have drained wetlands, mostly for agriculture Southern Canada and the U.S. have lost more than half of their wetlands
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Lakes and ponds are ecologically diverse Lakes and ponds are bodies of open, standing water Littoral zone = region ringing the edge of a water body Benthic zone = extends along the entire bottom of the water body Home to many invertebrates Limnetic zone = open portions of the lake or pond where the sunlight penetrates the shallow waters Profundal zone = water that sunlight does not reach Supports fewer animals because there is less oxygen
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A typical lake
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Lakes vary in their nutrients and oxygen Oligotrophic lakes and ponds = have low nutrient and high oxygen conditions Eutrophic lakes and ponds = have high nutrient and low oxygen conditions Eventually, water bodies fill completely in through the process of succession Inland seas = large lakes that hold so much water, their biota is adapted to open water
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Lake Baikal
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Groundwater plays a key role Groundwater = any precipitation that does not evaporate, flow into waterways, or get taken up by organisms Groundwater makes up one fifth of the Earth’s freshwater supply Aquifers = Porous sponge-like formations of rock, sand, or gravel that hold groundwater Zone of aeration = pore spaces are partially filled with water Zone of saturation = spaces are completely filled with water Water table = boundary between the two zones Aquifer recharge zone = any area where water infiltrates Earth’s surface and reaches aquifers
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A typical aquifer
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There are two categories of aquifers Confined or artesian = water-bearing, porous rocks are trapped between layers of less permeable substrate (i.e., clay) Is under a lot of pressure Unconfined aquifer = no upper layer to confine it Readily recharged by surface water Groundwater becomes surface water through springs or human-drilled wells Groundwater may be ancient: the average age is 1,400 years
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The Ogallala Aquifer The world’s largest known aquifer Underlies the Great Plains of the U.S. Its water has allowed farmers to create the most bountiful grain- producing region in the world
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Water is unequally distributed across Earth’s surface Different regions possess vastly different amounts of groundwater, surface water, and precipitation Many areas with high population density are water- poor and face serious water shortages
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Water is distributed unevenly in time, too Monsoon seasons bring concentrated storms Half a region’s annual rain may fall in a few hours People erect dams to store water
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Climate change will cause water shortages Climate change will cause Altered precipitation patterns Melting glaciers Early season runoff Intensified droughts Flooding Increasing probability that there will be still less water for more people
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How we use water We have achieved impressive engineering accomplishments to harness freshwater sources 60 % of the world’s largest 227 rivers have been strongly or moderately affected Dams, canals and diversions Consumption of water in most of the world is unsustainable We are depleting many sources of surface water and groundwater Water is becoming non-renewable resource
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Water supplies houses, agriculture, and industry Proportions of these three types of use vary dramatically among nations Arid countries use water for agriculture Developed countries use water for industry
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Different types of water use Consumptive use = water is removed from an aquifer or surface water body, and is not returned Non-consumptive use = does not remove, or only temporarily removes, water from an aquifer or surface water Electricity generation at hydroelectric dams
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Areas where water use exceeds supply
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US WATER USAGE
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We are depleting groundwater Groundwater is easily depleted Aquifers recharge slowly 1/3 of world population relies on groundwater As aquifers become depleted Water tables drop Salt water intrudes in coastal areas Sinkholes = areas where ground gives way unexpectedly Some cities (Venice, Mexico City) are slowly sinking Wetlands dry up
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Will we see a future of water wars? Freshwater depletion leads to shortages, which can lead to conflict 261 major rivers cross national borders Water is a key element in hostilities among Israel, Palestinians, and neighboring countries Many nations have cooperated with neighbors to resolve disputes
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Oceans cover most of the Earth’s surface The oceans influence global climate, team with biodiversity, facilitate transportation and commerce and provide resources They cover 71% of Earth’s surface and contain 97% of Earth’s surface water Oceans influence the atmosphere, lithosphere and biosphere
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The oceans contain more than water Ocean water is 96.5% water Plus ions of dissolved salts Evaporation removes pure water & leaves a higher concentration of salt Nutrients (nitrogen & phosphorus) Dissolved gas Nitrogen - diffusion Carbon Dioxide - diffusion Oxygen is added by plants, bacteria & atmospheric diffusion Salinity – the amount of dissolved inorganic solids in water Freshwater < 0.5 ppt Brackish 0.5 – 17 ppt Ocean 35 ppt (3.5 %)
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Ocean water is vertically structured Temperature declines with depth Heavier (colder saltier) water sinks Light (warmer and less salty) water remains near the surface Temperatures are more stable than land temperatures Water’s high heat capacity It takes much more heat to warm water than air Oceans regulate the earth’s climate They absorb and release heat Ocean’s surface circulation
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The ocean has several layers Surface zone Warmed by sunlight and stirred by wind Consistent water density Pycnocline = below the surface zone Density increases rapidly with depth Deep Zone = below the pycnocline Dense, sluggish water Unaffected by winds, storms, sunlight, and temperature
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Ocean water flows horizontally in currents Currents = the ocean is composed of vast riverlike flows Driven by density differences, heating and cooling, gravity, and wind Influence global climate and El Niño and La Niña Transport heat, nutrients, pollution, and the larvae of many marine species Some currents such as the Gulf Stream are rapid and powerful The warm water moderates Europe’s climate
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The upper waters of the oceans flow in currents
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Surface winds and heating create vertical currents Upwelling = the vertical flow of cold, deep water towards the surface High primary productivity and lucrative fisheries Also occurs where strong winds blow away from, or parallel to, coastlines Downwellings = oxygen-rich water sinks where surface currents come together
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Seafloor topography can be rugged and complex The seafloor consists of… Underwater volcanoes Steep canyons Mountain range The planet’s longest range is under water Mounds of debris Trenches Some flat areas
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A stylized bathymetric profile of the ocean
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