h0910meunit4pelagiczoneoceancurrentspowerpoint-091216131027-phpapp01

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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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