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WORLDS WATER SOURCES:
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Average # or people Love hustle & bustle The great outdoors Mid- Altitude
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Salinity Total amount of solid material dissolved in water
Typical salinity is 3.5% Six elements make up 99% of dissolved solids in seawater Fig. 5.12
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Salinity variations Open ocean salinity varies from 33 to 37 o/oo (PPT) Influx of freshwater lowers salinity Greater rate of evaporation raises salinity Salinity may vary with seasons (dry/rain)
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http://eesc. columbia. edu/courses/ees/climate/lectures/saltyatlantic
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Results in Less Water or More water??
Streams carry water to the ocean Seawater freezes in cold ocean areas Warm temperatures cause sea ice floats to liquify Rain, sleet, hail or snow falls directly on ocean Glacial ice breaks off (calves) into the ocean and melts Results in Less Water or More water??
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Sources of Ocean Salts Weathering and erosion of earth’s crust through rain runoff etc Dissolved from rocks below the sea floor through hydrothermal vents Volcanic ash
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Temperature Varies between -2 & 30 degrees (28-86 F)
Increases the metabolic rates of aquatic organisms Affects the rate of photosynthesis by aquatic plants and algae Increases the sensitivity of organisms to disease, parasites and pollution Raising water temperature increases decomposition rate of organic matter in the water depleting dissolve oxygen supplies
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Density Colder, saltier water sinks creating currents
Responsible for upwelling of nutrients to the surface upwelling demo
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Carbon dioxide – buildup in the air ends up in the ocean
This causes acidic conditions that prevent shells from forming! Acid Test: The Global Challenge of Ocean Acidification – YouTube Nitrates - Excess amounts of nitrates can cause algae to bloom wildly reducing oxygen levels for fish and sometimes causing their death (fertilizers!)
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Dissolved Gases Oxygen – most concentrated in colder waters, effects distributions of animals
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Transparency/Turbidity
can be affected by plant nutrients coming from sewage treatment or fertilizers. Suspended sediments in the coastal ocean may have come from re-suspension, coastal erosion, agricultural runoff of sediments and chemicals, and urban storm runoff. All of these elements, among others, affect the turbidity and transparency of the water a general indication of problems with algae, zooplankton, and silt
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Pressure Places limitations on physical structure of organisms
Ex. Fish in the deep sea lack a gas-filled bladder
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Epipelagic/Photic Zone
Enough light for photo-synthesis, most ocean life exists here 0-200m Mesopelagic/Twilight Zone – small amount of light, vertically migrating species here m Bathypelagic zone No light, many species have bioluminescence Abyssopelagic / Hadal Zone – deepest parts, no light, high pressure, low muscle mass, lack of color, no swim bladders
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pH Pure water = 7.0 (neutral)
Ocean Water = about 8.0 – 8.3 (slightly basic) Extremely high or low pH levels (above 11.0 and below 4.5) become lethal for most organisms
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