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The Oceans Nov. 18 Topics Thermohaline circulation –SST; –ocean water masses Wind-driven circulation –Wind-driven upwelling –Surface currents Mundus Subterraneus A. Kirchner, 1665
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Temperature 0m Stephens et al., NOAA, 2002
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Salt content of the oceans Source: leaching ions from crustal material. Global river dissolved load is ~0.1 ppt. Residence time: 10 8 yr Salinities for the open ocean fall in the range 33-38ppt (parts per thousand, mass per unit mass) http://omp.gso.uri.edu/doee/science/physical/salt5.gif
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Salinity 0m
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Water masses {sort of like air masses} http://earth.usc.edu/~stott/Catalina/images/weatherimages.jpg/airmasses.jpg
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Arctic sea ice http://www.ccpo.odu.edu/~arnoldo/ocean405/arcticdrift.jpg At 70N, Tromsö and Hammarfest ice-free year-round FebruarySeptember
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Deepwater formation processes http://puddle.mit.edu/~helen/oodc.html 1. preconditioning 2. Violent mixing 3. Sinking and spreading Where it happens
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Zonal average Temperature and salinity Levitus, 1984 Temperature salinity
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Transport units:
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Spatial distribution of deep and bottom water masses (Lynne Talley, SIO)
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Model of the overturning circulation Broecker, 1980s Reproduced in Ocean Circulation
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Wind-driven circulation
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Surface winds Trenberth et al., JPO, 1990
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tropical winds, rain From Ocean Circulation and Climate (OCC)
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Ekman transport
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Transports associated with winds
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Where water piles up:
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Mean surface currents
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Simulated sea surface temperature
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