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Published byPeter Ellis Modified over 9 years ago
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The Surface Currents Chapter 9
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Surface Currents Wind driven Coriolis effect 45º
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Surface Currents Ekman Spiral V. Walfrid Ekman ~100-150 m Ekman Transport 90
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Surface Currents Ocean Gyres
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Surface Currents Geostrophic Flow
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Pacific Ocean Currents North Equatorial North Pacific California Kuroshio Oyashio Alaska
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Pacific Ocean Currents South Equatorial West Wind Drift Peru (Humbolt) East Australia Equatorial Countercurrent Cromwell
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Atlantic Ocean Currents North Atlantic North Equatorial Gulf Stream Canary Florida Labrador East Greenland Norwegian
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Atlantic Ocean Currents West Wind Drift South Equatorial Brazil Benguela
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Indian Ocean Currents West Wind Drift South Equatorial West Australia Agulhas North Equatorial Equatorial Countercurrent
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Arctic Ocean Currents Clockwise gyre Not centered on North Pole
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Current Flow Current Speed 0.01 times average wind speed 0.1 – 0.5 m/sec Narrow straits Increase of speed Florida current Volume Sverdrups 1 Sverdrup = 1 million m 3 /sec
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Current Flow Western Intensification Western Boundary Current Eastern Boundary Current
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Eddies Meanders Surface or at depth Vary in size 10–100’s km in diameter Can alter surface flow pattern Retain properties
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Eddies Gulf Stream Rotational speed 0.51 m/sec (1 knot) Diameter 325 km (200 mi) Reach bottom Abyssal storms
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Convergence & Divergence
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Langmuir Cells
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Seasonal Zones
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Global Currents
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Milankovitch cycles 1. Shape of Earth’s orbit 100,000 years
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Global Currents Milankovitch cycles 2. Tilt of Earth’s axis of rotation 41,000 years
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Global Currents Milankovitch cycles 3. Circular revolution 23,000
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Recent History of Climate Change Minimum solar radiation 23,000 years ago Maximum land ice & minimum water temps 17,000 years ago Return to high solar radiation 12,000 years ago
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Recent History of Climate Change Younger Dryas event
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Recent History of Climate Change
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North Pacific Oscillations PDO Pacific Decadal Oscillation Yellow = Warm & dry Red = Cold & wet
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North Atlantic Oscillations NAO Pools of warm & cool surface water 4 to 10 years
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Measuring the Currents Highly sophisticated equipment:
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Measuring the Currents
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Current Meters
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Measuring the Currents Doppler current meter Emits sound of known frequency Measures frequency of returning echoes
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