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Pelagic zone
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OCEAN CURRENTS
current mass of water moving from one place to anotherlike a river within the ocean
importance:
moves drifting organisms from place to place plankton, disperse youngcarries eggs and larvae of organisms that have external fertilizationbrings food, oxygencarries away waste,pollutants
three types of currents surface currents thermohaline circulation (currents) wind-driven vertical currents (upwelling)
surface currentswind driven currentsoccur at surfacehorizontal currentscaused by friction between wind and water - wind pushes water
surface currentsCoriolis effectcauses moving objectsin northern hemisphereto veer clockwisecauses moving objectsin southern hemisphereto move counter-clockwise
surface currentsCoriolis effect
surface currentsgyre
massive circular system of wind-driven surface currentscover whole oceansclockwise inNorthern hemispherecounter-clockwisein Southernhemisphere
surface currentseddies = warm core ringsbreak off of currents and transport organisms elsewhere
thermohaline circulation (currents)
causes deep ocean circulationvertical currentstemperature and salinity cause water density differencesdue to density differences, water masses rise and fall
thermohaline circulation (currents)
salinity = density = water mass sinks temp. = density = water mass floats
thermohaline circulation (currents)
thermohaline circulation (currents)
when combined with surface currents, results in conveyor belt movement of water around globe
wind driven vertical currents = upwellingwind blows, moves water away, causes new water to rise up to replace it
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