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Inter-tropical Convergence Zone (ITCZ)
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Continental Effects: Monsoon
Winter: Ocean warmer than land Rising air over ocean Summer Land warmer than ocean Rising air over land
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Atmospheric Circulation
July in the Northern Hemisphere: Land warmer than sea; Low pressure over land January in the Northern Hemisphere: Sea warmer than land; Low pressure over ocean
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Wind-Driven Circulation (Gyre Circulation)
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Ekman Spiral: Friction + Coriolis
Wind + Friction Currents slow with depth Coriolis deflects current to right Summed over depth total transport 900 to right of wind = Ekman Transport
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Ekman Upwelling and Downwelling
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Biologically Productive Areas: Precipitation on Land Upwelling in Ocean
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Precipitation minus Evaporation
P-E = freshwater input to ocean Patterns follows the ascending and descending branches of atm circulation cells sea surface salinity
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Sea Surface Salinity (per mil or psu)
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Thermohaline Circulation (Conveyor Belt)
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Hydrothermal Vents at the Sea Floor
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