Pidwirny, 2004 Peixoto and Kettani, 1973 Source: Natural Resources Canada Percentage of Population with Access to Water Supply Services Solutions for Depletion: Desalination • Desalinization removal of salt from seawater to create freshwater • Perfecting this technology would mean the oceans could provide us with unlimited freshwater. • Most of the world’s 7,500 desalination plants are in wealthy oil states of the Middle East, where water is scarce enough to make desalination economically feasible. How we Use Water • Consumptive use water is removed from an aquifer or surface body, and not returned (most agricultural, industrial, and some residential use) • Nonconsumptive use = removal of water is only temporary (passing water through a hydroelectric dam) Agricultural Water Use • Agriculture = 87% of world’s consumptive use of water • Global consumption has risen in tandem with irrigation. Disappearance of the Aral Sea (Kazakhstan and Uzbekistan) The Aral Sea was once the fourth largest freshwater body in the world, but has all but disappeared Groundwater Extraction • 1 in 3 humans relies on groundwater for drinking. • 99% of the rural U.S. & much of Canada relies on groundwater for drinking. • Extraction from aquifers is increasing, especially in developing nations whose agriculture intensified with green revolution. Aquifers • Aquifer = a porous spongelike layer of rock, sand, or gravel that holds groundwater • Confined or artesian aquifer = water under pressure, trapped within impermeable layers (often clay) • Unconfined aquifer = water under less pressure; no overlying impermeable layer • Aquifer recharge zone = geographic area where water infiltrates soil and recharges aquifer. Groundwater and Aquifers Impacts of Water Mining • When water is mined, ground may suddenly collapse in sinkholes. Other impacts: Slow subsidence (Venice, Mexico City) Saltwater intrusion into drinking water Wetland destruction Figure 14.14 Surface Diversion • Colorado River water is heavily diverted today from a series of dams, mostly for agriculture. Are the Great Lakes next? Flood control • We build dikes and levees to prevent floods when river levels rise. • Flood control has saved many towns and crops from ruin. • But long term, flood control can be self-defeating: • Forces floodwater to stay in channel, creating risk of catastrophic overflow, rising river base due to deposition or dike break downstream • Deprives farmland of nutrients that floods bring; decreases soil productivity Dams • We build dams blocking the flow of rivers in order to: –•Prevent floods –•Generate electricity –•Provide drinking water –•Provide irrigation • 45,000 dams over 15 meters high have been built in the world. • Few major rivers today are not dammed. Benefits and costs of dams Figure 14.11 Sedimentation and burial of archaeological sites are cited by critics Photo: Greg Baker, Guardian Precipitation Glaciers Groundwater Surface water • Most intensively farmed and irrigated region in Canada • 1/3 of the province’s sales of agricultural products •90 % of all water in the Oldman and its tributaries to irrigated agriculture •food processing becoming bigger industry - requires high quality water resources •City of Lethbridge growing quickly •Master Apportionment Agreement 50% of South Saskatchewan’s water must enter Saskatchewan •maximum daily production is 120 million litres of water from Oldman •6% of Canadians not served by wastewater treatment •41% now receive tertiary treatment Lethbridge & Calgary apply UV disenfection after tertiary Treatment (sludge used as fertilizer) Types of Pollution: Pathogens • Waterborne disease from viruses, bacteria, etc., contributes to 5 million deaths per year. • Diarrhea: 4 billion cases/year, 2.2 million deaths • Intestinal worms: 1 in 10 people in developing world • Blindness from trachoma: 6 million people • Schistosomiasis from blood flukes: 200 million people See: http://www.trachoma.org/ +2.5 to +3.3C 3 to 7% Alberta Population 1991: 2,545,553 2001: 2,974,807 A 16% increase in 10 years Often locate near water bodies for: •Transportation •Clean Water Source •Cooling •Effluent Discharge Contamination of groundwater or large water bodies leads to decades, centuries or more of pollution! •17% of Canadian municipalities report a water availability problem •10% of Canadians rely exclusively on groundwater (population growth is problematic in these areas) •Canadians use more water per capita than anyone else in the world and our water is the cheapest 1. Correct leakage (thousands of L) 2. Use efficient toilets and washers 3. Take shorter showers 4. Don’t over-irrigate lawn & garden 5. Be aware of water use POINT SOURCES •Septic systems •Leaky petroleum pipelines/tanks •Industrial chemical leaks, spills & discharge •Municipal landfill sites •Livestock waste •Leaky sewer lines •Wood preservation chemicals •Tailings in mining areas •Fly ash from coal-fired power plants •Sludge disposal areas at petroleum refineries •Sewage or sewage sludge fertilization •Graveyards •Road and highway salt & salt storage runoff •Wells for disposal of liquid wastes •Highway or railway accident spills •Coal tar at old coal gasification sites •Asphalt production and equipment cleaning sites Distributed Sources of Water Pollution •Fertilizers on agricultural land •Pesticides on agricultural land and forests •Lawns, gardens and golf courses •Phosphates from car washes & laundry •Contaminants in rain, snow, and dry atmospheric fallout •71% of Earth’s Surface •Reservoir for CO2 •Temperature regulator •Habitat for 250 000 species •Dilution of Pollutants •Resources •Species rich •Dampen wave energy •Food and shelter for fish and invertebrates •Antimicrobial and antiviral compounds AN ECOSYSTEM UNDER THREAT - rising water temperature - land reclamation - siltation - tourism - rising seas Declining concentrations of photosynthetic pigments within the zooxanthellae Partially enclosed bodies of water formed where freshwater from rivers and streams flows into the ocean Transition: FRESHWATER to SALTWATER Photo: Campbell River Estuary Nature Conservancy of Canada Tidal, sheltered, highly productive bodies of water Varied in form: bays, lagoons, inlets etc. Shore birds, fish, crabs and lobsters, marine mammals, shellfish, marine worms, sea birds, and reptiles 1. Euphotic Zone •Upper 100 – 200 m •Sunlight permits photosynthesis phytoplankton whales zooplankton small fish tuna mackeral seals decomposer & scavenger 2. Bathyl Zone (200m – 2km) •Twilight •Low density of large animals (eg. sperm whales, giant squid) 3. Abyssal Zone (2km+) •Very little light penetration •Animals adapted to darkness Benthic Environment = ocean floor http://msnbc.com/news/674647.asp?0sl=-42&cp1=1 1. Littoral Zone •High nutrient availability •Available sunlight •Most productive zone of lake •Rooted plants (producers) •Fish, frogs, turtles, worms, crustaceans and insects 2. Limnetic zone •Further from shore, few or no rooted plants •Phytoplankton, zooplankton •Fish (some large) OVERTURN 4°C OLIGOTROPHIC EUTROPHIC MESOTROPHIC 3. http://users.rcn.com/jkimball.ma.ultranet Wetland Environments •Cover 14 to 18% of Canada •Mainly just to the south of treeline in discontinuous and sporadic permafrost •Pockets further north •Major carbon sink •Potential future source of greenhouse gases •Hydrophyllic vegetation present due to water table at or above mineral soil Bog • • Sphagnum moss dominated Receives nutrients only from precipitation Fen • • A peatland receiving nutrients from mineral soil below Flora is more abundant and diverse, including sedges, grasses, shrubs and even trees (tamarack) Swamp • • • A wooded wetland May develop into a peatland Coniferous and deciduous trees, shrubs, herbs and mosses Marsh • • Periodically inundated wetland (fresh or salt water) Little peat accumulation Why does peat accumulate ? •Production by plants exceeds decomposition •Abundant growth due to available moisture during growing season •Preservation of plants (cool conditions) •Saturated conditions - slow, anaerobic decomposition by methanogenic bacteria •Release of methane rather than CO2 Salmonid Species Chinook Chum Trout Coho Pink Cutthroat Sockeye (Steelhead) Dolly Varden Pacific Cod Rockfish Flounder Herring Eel Commercial Fishing • $500 million yr-1 industry (salmon) • 8 million fish caught annually Aquaculture •$400 million yr-1 •Mainly salmon Shellfish •clams and oysters Shellfish Shrimp, scallops, crabs Birds Eagle, vulture, heron, cormorant, swan, goose, grebe, duck, hawk, falcon, grouse, ptarmigan, quail, crane, plover, sandpiper, gull, finch, woodpecker, owl, jay, raven, swallow wren, warbler, sparrow, blackbird Marine mammals Whales, porpoises, dolphins, sea otters, seals, sea lions http://www2.news.gov.bc.ca/nrm_news_releases/2002AGF0020-000827.htm Closures of shellfish harvesting •sewage contamination •high levels of dioxins and furans Quotas are lower every year FINFISH: Cod, haddock, plaice, flounder, herring, mackerel, tuna, salmon and capelin INVERTEBRATE: Shrimp, lobster, crab, scallops, clams Pits animal rights activists against fishing industry Photo: CBC (also leads to a decline in sea bird populations) Source: NCAR Annual average surface water temperature in the Labrador Sea vs. North Atlantic Oscillation •Falling temperatures: the result of increased ice sheet melting? NAO? change in thermohaline circulation? •Salinity is also on the decrease •Temperature and salinity changes alter the spatial distribution and health of a species •These changes are thought to be related to the collapse of the cod fishery (with overfishing and predation) •Damages ocean floor environments •Catch too many fish/ too young YEAR TONNES VALUE 1/3 of suitable shellfish sites are closed due to contamination Lobster Dispute (Nova Scotia) •1760 Treaty between Chief Augustine (Micmac) and King George •Guaranteed aboriginal rights to use resources •Dispute with non-native fishers in regulated industry •Government allows just 40 traps during off-season: confiscated boats and traps •Violence escalated in ’99/’00: police rammed boats, fires set by both sides Cause: mismanagement of lobster fishery • Over 1 million km2 of shelf waters • Most of food for Canadian Inuit • ¼ of productivity of Atlantic/Pacific due to thick sea ice • Highest productivity near polynyas and between shorefast and drifting pack ice Source: Yngve Kristoffersen •Input of water is from the Norwegian Current (warmer and more saline - NA drift) •Beaufort Sea Gyre clockwise due to polar easterlies •Cold, relatively fresh water leaves the Arctic Ocean via the Fram Strait (becomes the East Greenland Current) •Net export of water (little evaporation) Differences from fresh water •Freezes between -1.65°C and -1.92°C (more heat loss required to freeze) •Maximum density is freezing point (water column is destabilized) Mixed layer of several metres required for freeze-up ! Pack Ice Far from shoreline (moves due to currents and winds) Shorefast Ice: Close to shore but still moves up and down Ice foot: Frozen solid to the shore (unaffected by tides), formed by wave action The ice foot is separated from shorefast ice by a tidal crack International North Water Polynya Study http://www.fsg.ulaval.ca/giroq/now/polyb.jpg Frazil forms near the surface in the mixed layer around suspended particles (centres of nucleation) In calm water: Frazil accumulates on the surface forming grease ice In turbulent water: Frazil freezes into balls/pans which freeze together when the ice dampens the waves When there is stable ice cover, elongated crystals grow downward Limits exchange of sensible and latent heat (lowers temperature and precipitation) Increases albedo (decreases temperature) Limits exchange of oxygen and carbon dioxide Blocks light, virtually eliminating photosynthesis Restricts range of some marine mammals (eg. whales) but extends the range of others (sea ice is important to seals) •Semi-permanent areas of open water •Remain unfrozen despite high arctic climate Latent Heat Polynyas: Currents or winds remove new ice Sensible Heat Polynyas: Warm water continually brought upward to a site •Polynyas are biologically important •Oxygen exchange with the air allows marine life to continue throughout the winter •Nutrients brought by currents maintain an active food chain in the winter •Marine mammals like walrus and whales can live here year-round •Important sites for northern hunting culture Arctic sea-ice extent decreased by 2.9% per decade (1978-1996) Sea ice has thinned Northwest Passage new route from Asia to Europe? •Mainly subsistence hunting/fishing •Commercial fishery includes: - Arctic Char ($1.2 million yr-1) - Turbot ($ 1 million yr-1) - clams, shrimp, scallops (local) Arctic Char (Balena mysticetus) “Greenland Right Whale” •A baleen whale: Filters zooplankton and krill through a mesh of thin, flexible, bony plates up to 3m long, suspended from the upper jaw •20m in length; weighs up to 70 tons Females are larger than males Distribution: Between 55°N and the permanent polar pack •Original population around 50000 Mid 1800’s: 5 populations near extinction 1970’s: 4500 Today: 8500 •Spend winter around polynyas •Hide from killer whales around ice floes •Canada withdrew from the IWC in 1982 •Cetacean Protection Act (Canada) Inuit: 1 bowhead per year (1995) Delphinapterus leucas “White Whale” •Most common whale in Canadian Arctic •4-5m in length, 540-765 kg •Nutrition: Bottom-dwelling fish, benthic invertebrates, squid & arctic cod •Lifespan: Approximately 25-30 years Population: 10000 in Lancaster Sound 10000 in Beaufort Sea 1500 in east Hudson Bay 25000 in west Hudson Bay Beluga whale carcasses are toxic waste! 20% have cancers at death Toxins accumulate most in fatty tissues List of toxins include chemicals banned for decades Monodon monoceros •Spiralled tusk – function uncertain (mating?) •Narwhals are 5m long + 2m tusk •600 -1200 kg (males larger) •More restricted distribution beluga whale: Many in Lancaster Sound area. Seldom seen south of the Arctic Circle Migratory: winters in heavy pack ice of Baffin Bay and in the Davis Strait – some in mouth of Hudson Strait • Migrate northward in summer • Narwhals dive more deeply than beluga whales Nutrition: Crustaceans, molluscs, squid, shrimp, Arctic Cod Population: 20000 in Lancaster Sound, 2000 in north Hudson Bay Hunting: Can only be hunted by Inuit for subsistence and domestic purposes (quota since 1977) • They are hunted for their tusks and for muktuk Orcinus orca •Hunt in packs of 3-40 animals Location: Throughout world’s oceans but most abundant in cool, temperate waters. In Arctic, they are found from Davis Strait to Lancaster Sound and may penetrate Hudson Bay. Killer whales like to avoid heavy pack ice Migratory: Follow migration herds of seals; migrate south in winter Nutrition: Eat fish, squid, seabirds, seals (dislodge them from beneath ice floes), other cetaceans Size: Males 6-9m, females 4-5m Lifespan: 40-50 years