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Do Now 05.19.10 What causes the seasons?
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Objective State the reasons for global wind patterns and ocean currents.
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Coriolis effect: deflection of wind and ocean currents caused by the Earth’s rotation Winds in N. Hemisphere flow to the right Winds in S. Hemisphere flow to the left
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jet stream: narrow belt of strong, high speed air height about 10 to 15 km above N. and S. Hemispheres closely related to weather (2) global winds
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http://www.weatherimages.com/data/imag192.html (current position)
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anemometer: instrument that measures wind speed
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wind vane: measures wind direction
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*always points into the wind wind This is an easterly wind because it is blowing from the east
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Doldrums
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Uneven heating of air Uneven heating of air Uneven heating of air Coriolis Effect Coriolis Effect Coriolis Effect
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Ocean Currents Currents are the steady movement of water in the ocean
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Ocean Currents Currents are the steady movement of water in the ocean surface currents move on or near the surfacesurface currents move on or near the surface
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Ocean Currents Currents are the steady movement of water in the ocean surface currents move on or near the surfacesurface currents move on or near the surface driven by the wind
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Ocean Currents Currents are the steady movement of water in the ocean surface currents move on or near the surfacesurface currents move on or near the surface driven by the wind deep currents occur deep beneath the surfacedeep currents occur deep beneath the surface
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Ocean Currents Currents are the steady movement of water in the ocean surface currents move on or near the surfacesurface currents move on or near the surface driven by the wind deep currents occur deep beneath the surfacedeep currents occur deep beneath the surface caused by differences in the density of the water
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Ocean Currents Currents are the steady movement of water in the ocean surface currents move on or near the surfacesurface currents move on or near the surface driven by the wind deep currents occur deep beneath the surfacedeep currents occur deep beneath the surface caused by differences in the density of the water move very slowly
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Surface Currents Wind provides energy to move large masses of water
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Surface Currents Wind provides energy to move large masses of water upper layer of water moves the fastest
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Surface Currents Wind provides energy to move large masses of water upper layer of water moves the fastest velocity decreases with depthvelocity decreases with depth
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Surface Currents Wind provides energy to move large masses of water upper layer of water moves the fastest velocity decreases with depthvelocity decreases with depth below 100m most surface currents are undetectablebelow 100m most surface currents are undetectable
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Surface Currents Surface currents are controlled by three factors
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Surface Currents Wind belts
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Surface Currents Wind belts Trade Winds are located just north and south of the equatorTrade Winds are located just north and south of the equator
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Surface Currents Wind belts Trade Winds are located just north and south of the equatorTrade Winds are located just north and south of the equator push currents westward across tropical latitudes
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Surface Currents Wind belts Trade Winds are located just north and south of the equatorTrade Winds are located just north and south of the equator push currents westward across tropical latitudes Westerlies are located in the middle latitudesWesterlies are located in the middle latitudes
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Surface Currents Wind belts Trade Winds are located just north and south of the equatorTrade Winds are located just north and south of the equator push currents westward across tropical latitudes Westerlies are located in the middle latitudesWesterlies are located in the middle latitudes push eastward in the northern hemisphere
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Surface Currents Wind belts Trade Winds are located just north and south of the equatorTrade Winds are located just north and south of the equator push currents westward across tropical latitudes Westerlies are located in the middle latitudesWesterlies are located in the middle latitudes push eastward in the northern hemisphere in the south, pushes West Wind Drift completely around the world
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Surface Currents Wind belts Trade Winds are located just north and south of the equatorTrade Winds are located just north and south of the equator push currents westward across tropical latitudes Westerlies are located in the middle latitudesWesterlies are located in the middle latitudes push eastward in the northern hemisphere in the south, pushes West Wind Drift completely around the world earth’s largest currentearth’s largest current
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westerlies
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Surface Currents Coriolis effect: deflection of the earth’s winds and ocean currents
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Surface Currents Coriolis effect: deflection of the earth’s winds and ocean currents caused by the rotation of the earthcaused by the rotation of the earth
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Surface Currents Coriolis effect: deflection of the earth’s winds and ocean currents caused by the rotation of the earthcaused by the rotation of the earth Gyres: huge circles of moving water
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Surface Currents Coriolis effect: deflection of the earth’s winds and ocean currents caused by the rotation of the earthcaused by the rotation of the earth Gyres: huge circles of moving water caused by the combination of wind belts and the coriolis effectcaused by the combination of wind belts and the coriolis effect
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Surface Currents Coriolis effect: deflection of the earth’s winds and ocean currents caused by the rotation of the earthcaused by the rotation of the earth Gyres: huge circles of moving water caused by the combination of wind belts and the coriolis effectcaused by the combination of wind belts and the coriolis effect clockwise in the northern hemisphereclockwise in the northern hemisphere
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Surface Currents Coriolis effect: deflection of the earth’s winds and ocean currents caused by the rotation of the earthcaused by the rotation of the earth Gyres: huge circles of moving water caused by the combination of wind belts and the coriolis effectcaused by the combination of wind belts and the coriolis effect clockwise in the northern hemisphereclockwise in the northern hemisphere counterclockwise in the southerncounterclockwise in the southern
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Surface Currents Third factor affecting currents
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Surface Currents Third factor affecting currents continentscontinents
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Surface Currents Third factor affecting currents continentscontinents deflect and divide currents
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Surface Currents Equatorial currents: westward moving warm-water currents
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Surface Currents Equatorial currents: westward moving warm-water currents Located in all three oceansLocated in all three oceans
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Surface Currents Equatorial currents: westward moving warm-water currents Located in all three oceansLocated in all three oceans currents in the northern hemisphere
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Surface Currents Equatorial currents: westward moving warm-water currents Located in all three oceansLocated in all three oceans currents in the northern hemisphere swift warm water moves north in the western side of the oceansswift warm water moves north in the western side of the oceans
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Surface Currents Equatorial currents: westward moving warm-water currents Located in all three oceansLocated in all three oceans currents in the northern hemisphere swift warm water moves north in the western side of the oceansswift warm water moves north in the western side of the oceans Cool currents move south in the eastern sideCool currents move south in the eastern side
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Surface Currents examples of warm water currents:
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Surface Currents examples of warm water currents: Gulf streamGulf stream
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Surface Currents examples of warm water currents: Gulf streamGulf stream Japan currentJapan current
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Surface Currents examples of warm water currents: Gulf streamGulf stream Japan currentJapan current East Australia currentEast Australia current
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Surface Currents examples of warm water currents: Gulf streamGulf stream Japan currentJapan current East Australia currentEast Australia current Brazil currentBrazil current
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Surface Currents examples of cool water currents:
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Surface Currents examples of cool water currents: West Wind driftWest Wind drift
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Surface Currents examples of cool water currents: West Wind driftWest Wind drift California currentCalifornia current
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Surface Currents examples of cool water currents: West Wind driftWest Wind drift Californa currentCaliforna current Canary currentCanary current
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Surface Currents examples of cool water currents: West Wind driftWest Wind drift California currentCalifornia current Canary currentCanary current Peru currentPeru current
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Deep Currents move more slowly than surface currents
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Deep Currents move more slowly than surface currents produced as cold, dense water sinks below warmer water
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Deep Currents move more slowly than surface currents produced as cold, dense water sinks below warmer water from cold polar regions towards the equatorfrom cold polar regions towards the equator denser because of higher salinitydenser because of higher salinity
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