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Published byDiane Cummings Modified over 9 years ago
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Coastal Upwelling Equatorward winds along a coastline lead to offshore Ekman transport Mass conservation requires these waters replaced by cold, denser waters Brings nutrients to the surface increasing rates of primary production Creates dynamic height gradients - currents
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Coastal Upwelling
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CalCoFI Cruise 9804
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Coastal Upwelling Changes Density Line 90
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Density & Currents for Line 90 Negative currents to south
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Primary Production Phytoplankton h CO 2 O2O2 PlantsNUTS Light, carbon & nutrients make plants & O 2
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Respiration & Remineralization remineralizers h CO 2 O2O2 PlantsNUTS Biological processes consume plants & O 2 to make CO 2 & nutrients
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Euphotic Zone Euphotic Zone – PP happens Aphotic Zone - Respiration & Remineralization Depth of Euphotic Zone is f(water clarity) 100% Light1% Light
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Euphotic Zone Defined as the depth where the light = 1% of the surface value A function of plant biomass or chlorophyll concentration Varies from 10 to 130 m Typically, Z eu = 3 * Secchi depth
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CalCoFI Light Profiles % surface light Depth (m) Secchi = 7 m Secchi = 18 m
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Primary Production Phytoplankton h CO 2 O2O2 PlantsNUTS Light, carbon & nutrients make plants & O 2
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Facts & Predictions CO 2 will not be limiting In euphotic zone … – NUTS will be consumed – O 2 & plants will grow (high chlorophyll) In aphotic zone … – Remineralization produces CO 2 & NUTS – Consumes O 2 & plants
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Facts & Predictions KEY: Upper layer biology is controlled by supply of nutrients to euphotic zone Upwelling is dominate process regulating primary production
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Density & Currents for Line 90 Negative currents to south
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NUTS for Line 90
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Line 90 Results In euphotic zone … – NUTS are low – O 2 & plants are high (O 2 is supersaturated) In aphotic zone … – NUTS are high – O 2 & plants are low Pattern follows physical inflow
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CalCoFI Cruise 9804
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Link to Physical Process April 1978 AVHRR - SST CZCS Chlorophyll SST Chl
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Coastal Upwelling
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The Upwelling Conveyor Belt Highest NUTS & CO 2 High NUTSLow NUTS High ChlLow ChlLower Chl Sinking Flux of Carbon
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Biological Water Masses Residence time in euphotic zone controls nutrient concentrations Source characteristics are also important
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Primary Production Simple light-NUT model explains basic features regulating primary production Physical processes drive nutrient supply to euphotic zone & primary production Concept of “upwelling conveyor belt” Water mass characteristics
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