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Surface circulation Deep ocean circulation
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Surface currents General pattern
Gyres created by wind and modified by Coriolis effect Water moves horizontally Selected other currents
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Trade Winds (grey) and Westerlies (green) create gyres (purple)
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Gyres General circular flow of surface currents
Western boundary currents (intensified) Eastern boundary currents Equatorial currents
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Ekman transport Driven by winds Modified by Coriolis
Currents veer 90 degrees to the right or left of the wind (depending on hemisphere) Water piles up in center of gyres
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Ekman transport – note direction of wind over water and direction of net transport of top 100 meters of water
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Ekman transport (version 2) - note arrows spiraling down – progressively smaller and changing direction down to 100 meters depth kman Transport
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Geostrophic circulation
Driven by gravity Modified by Coriolis effect Water flows down away from center of hill in center of gyre, but bends due to Coriolis
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Geostrophic circulation imagine hill of water at center of gyre
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Upwelling and downwelling along a coast
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El Nino circulation – note position of warm and cold surface water
Top – “normal” Middle – El Nino Bottom – La Nina
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Deep ocean circulation
THERMOHALINE (temp and salinity) Density driven Formation of distinct water masses Sinking at poles and movement toward equator Different from surface ocean circulation
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Deep ocean circulation - simplified
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Conveyor belt model of deep ocean circulation
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Closer look at Gulf Stream
Flows like a river with meanders Meanders pinch off and become rings Warm core eddies Cold core eddies
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