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Properties of Ocean Water
Chapter 20-1 Properties of Ocean Water
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Pure Water Colorless Odorless Tasteless
Ocean water contains solids and gases dissolved within
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Dissolved Gases Most abundant gases in ocean: Nitrogen N2 Oxygen O2
Carbon dioxide CO2
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How do they get there? From streams and rivers Volcanic eruptions
Organisms that live there Directly from atmosphere
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Temperature Dissolve more readily in cold water
Pop goes ‘flat’ quicker on warm days Cold areas dissolve gases more than tropical areas
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Temperature Cold areas hold onto CO2
Warm areas release more CO2 into the atmosphere
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Carbon Sink Oceans have 60% more carbon than atmosphere
Important to regulate climate. Why?
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Dissolved Solids 3.5% of oceans mass Sea salts
Halite makes up 85% of solids
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Where do they come from? Volcanic eruptions
Chemical weathering on land Chemical weathering between water and rocks
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Salinity Salinity – Measure of amount of dissolved salts and other solids
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Salinity Factors that change: Evaporation Precipitation
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Surface Water Distributes heat from 100 – 300 m Tropical: 30 C
Polar: -1.9 C Ocean water can freeze at this temperature
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Pack Ice Pack ice – floating sea ice 5 m thick
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Thermocline Thermocline – layer in ocean where water temperatures drop faster than in other areas
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Deep Water 2 C Colder = denser Controls deep water currents
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Density Salinity and temperature Denser than pure water
Denser - colder
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Color Determined by the way it absorbs or reflects sunlight
Blue light reflected Phytoplankton can affect color
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