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Published byElisabeth Jones Modified over 8 years ago
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Currents
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Surface currents – Develop from friction between the ocean and the wind that blows across the ocean surface – 2 Types: warm and cold
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Gyres Gyre: large circulation of water within an ocean basin (ie. Atlantic, pacific, or indian ocean basin) Wind main force that generates surface currents – Coriolis effect is a factor that influences currents – Coriolis effect: the deflection of currents away from their original course as a result of Earth’s rotation – Northern hemisphere: clockwise – Southern hemisphere: counterclockwise
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Currents & Climate Currents moderate temperatures on land by bringing warm water from the equator and cold water from the poles
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Upwelling Wind induced vertical water movement Upwelling: the rising of cold water to replace warmer surface water that has been displaced by wind Brings dissolved nutrients, such as nitrates and phosphates, to the ocean surface
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Waves
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Wave Characteristics Most ocean waves derive their energy from the wind Wave height: the vertical distance between trough and crest Wavelength: horizontal distance between two successive crests or troughs Wave period: the times it takes for one wave to pass a certain point
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Wave Characteristics The height, length, and period that are eventually achieved by a wave depend on three factors – Wind speed – Length of time wind is blowing – & fetch; the distance the wind has traveled across open water.
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Wave Motion Circular orbital motion allows energy to move forward through the water while the water particles that transmit the wave move around in a circle
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Circular orbital motion Water particles move in circle Movement up and down and Back and forth Fig. 8.4
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Tides
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The regular changes in the elevation of the ocean surface Tides form from the gravitational attraction exerted upon different parts of the Earth’s surface by the moon, and by a lesser extent by the sun.
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Tidal Patterns Diurnal: a single high tide and a single low tide each tidal day Semidiurnal: two high tides and two low tides each tidal day Mixed: two unequal high water level heights, low water heights, or both
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Shoreline Features and Processes
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Shoreline Processes and Features Many shoreline features result from wave erosion, deposition, and transport of sediments Longshore currents: the current that flows parallel to the shore and moves a large amount of sediment along the shore
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Erosional Features Sea Cave, Sea arch, and sea stack – Listed in order of increasing erosion
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Depositional Features Examples: spits, tombolos, and barrier islands Barrier island – Example: North Carolina outer banks
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Stabilizing the Shore Structures are built along beaches to prevent erosion of sediment along the coast – Examples include groins, breakwaters, and seawalls Beach nourishment: the artificial addition of large quantities of sand to the beach system
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