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Ocean Circulation Tyburn Marine Biology - Spring 2019
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Ocean currents have a big effect on the weather!
The Scilly Isles – only 30 miles off the coast of Cornwall, England (lat 50o!) but in the warm Gulf Stream! Ocean currents have a big effect on the weather! Iceland Weather…
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The Mediterranean Sea, seen from the Space Shuttle, looking toward the east
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GYRE – The flow around the periphery of an ocean basin (from gyros = a circle)
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Surface Winds drive the initial surface gyres…
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But it’s more complicated!
Four Forces – surface winds, the Sun’s heat, Coriolis Force, and Gravity – determine the exact patterns for ocean currents
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North Atlantic Gyre Coriolis Force effects
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Coriolis Forces play an even more important role for ocean currents than for atmospheric winds – because these small but persistent forces have more time to act on slower-moving ocean currents! Video1! Video2!
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The Ekman “spiral”
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Overall water column movement is about 45o to RIGHT of winds (N. Hem)
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Wind North Atlantic Water!
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“center” of hill!
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The Result…
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Global Ocean SURFACE Currents
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Western Boundary Currents – the fastest on Earth!
A Sverdrup (sv) = 1 million m3 per second!
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The Gulf Stream
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The Gulf Stream
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Gulf Stream “eddies”
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A photo mosaic of several day’s IR data
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An eddy off the coast of Japan!
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Transverse Currents – provide the links for the northward and southward flowing currents
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Today will be hazy, hot, and humid in Annapolis …
Today will be hazy, hot, and humid in Annapolis ….summertime weather is affected by ocean and atmosphere currents
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Equatorial Upwelling
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Coastal Upwelling (or subsidence
Coastal Upwelling (or subsidence!) is caused by the Coriolis transport of water near the surface (where the angle is nearly 90 degrees)
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Growth of phytoplankton in the nutrient-rich waters where upwelling is taking place off the California coast.
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caused by winds that blow steadily across a wide ocean area
Langmuir Circulation caused by winds that blow steadily across a wide ocean area
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A “non-El Nino” year!
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El Nino year has unusually warm eastern Pacific waters!
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A quick return to cooler conditions
Peak El Nino
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Thermohaline Circulation a VERTICAL, density-driven ocean circulation!
Mixing of equal-density water from points a and b would produce MORE dense water at point c – it would SINK!
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Basin-driven vertical circulations – the Strait of Gibralter between Spain and Morocco
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“Classic” Thermohaline circulation
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Atlantic Ocean Water Layers and Sources
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Convergence and Divergence of Surface Waters
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Measuring Ocean Currents
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1992 “Rubber Ducky” accident
SOFAR float (11,500 ft!)
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Current Measuring Devices
A “Woodhead” seabed drifter
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Ekman Flow meter
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A Slocum Glider – uses energy from gravity, buoyance, heat and batteries to “swim” for months and report info about currents from it’s GPS
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