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Published byErica Day Modified over 9 years ago
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Oceans
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Formation of the Ocean After the Earth cooled, water vapor in the atmosphere condensed, causing rain to fill the first ocean.
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Current Divisions Four major divisions: Arctic Ocean Indian Ocean Atlantic Ocean Pacific Ocean
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Ocean Water Salinity: measure of the amount of dissolved solids in a given amount of liquid
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Ocean Water The salinity of ocean water is 35 g per 1000 g. Salt makes up the majority of dissolved solids.
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Ocean Water Factors that affect salinity: Evaporation Circulation Freshwater inflow
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Movement of Ocean Water Surface currents: stream like movement of water at or near the surface of the ocean
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Movement of Ocean Water Surface currents affect climate by cooling or heating the coastline.
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Movement of Ocean Water Deep currents: streamlike movement of water far below the surface Deep and surface currents are the result of convection.
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Tides Tides are daily movement of ocean water that change the level of the ocean’s surface.
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Tides High tide and low tide depend on the position of the moon as it revolves around the Earth.
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High Tides The moon’s pull is strongest on the side facing the moon. This causes a bulge on the side facing the moon and directly opposite.
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Tide Variations The sun also affects tides. The tidal range is the difference between low and high tide.
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Spring Tide When the sun, moon and Earth are aligned, spring tides occur. Maximum daily tidal range
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Neap Tide When the sun, Earth and moon make a 90º angle Minimum daily tidal range
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