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To identify, describe and list factors that control ocean currents
Purpose: To identify, describe and list factors that control ocean currents To explain how ocean currents affect climate in San Diego and the world
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Warm-up Imagine you are stranded on a desert island in the North Pacific Ocean. You stuff a distress “help” message in a bottle and throw it in the ocean, hoping someone in San Diego will get it. Is it possible someone in San Diego will find your message and send help? Explain your answer.
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Light decreases with depth! Temp also decreases with depth!
THERMOCLIME: transitional ocean layer 3 Layers : Warm Upper Thermocline Cold Lower
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Surface Currents Are stream like movements of water at the ocean’s surface. They are caused by the prevailing winds Circulate thousands of miles across entire oceans
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Surface Currents are influenced by:
Global winds The Coriolis Effect Continental deflections
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Surface winds (purple arrows) create surface currents (red)
The Trade Winds move currents east to west along the Equator The Westerlies move currents west to east in mid-latitudes
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Ocean currents distribute heat throughout the depths of the ocean
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The Coriolis Effect Winds, ocean currents and moving objects appear to move in curved paths as the Earth rotates beneath
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Coriolis Effect Demonstration: Northern Hemisphere
Draw 2 circles Rotate the paper counterclockwise Prediction: Draw a straight line from a to b. Describe the result Draw a straight line from c to d. Describe the result b d c
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Continents cause surface currents to change directions
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Surface currents affect climates of the world
The Gulf Stream brings warm water from the Equator to northern Europe Warmer climates result in latitudes that are similar to Canada
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Cold water from the north is carried southward by the California Current
The cold water current keeps the climate comfortable along the West Coast all year
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What upwelling is The rising of cold water from deeper layers which replaces warmer surface water along a shoreline Upwelling Animation
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What upwelling does Brings more dissolved nutrients such as nitrates and phosphates to the ocean surface Responsible for the booming marine life population off the coast of California, Peru, and western Africa
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How upwelling happens Wind moves blows along the shore
Coriolis Effect causes warm surface water to move away from shore. Cold water rises up from below to fill in the area the warm water leaves
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El Nino: is the change in the location of warm and cold surface water every 2-7 years results in worldwide weather changes causes heavy rains and mudslides in California and droughts in other regions
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Normal weather patterns occur when warmer water is found in the western pacific near Asia
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During El Nino, purple shows warmer water located near America in the eastern pacific.
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Weather patterns across the USA and the world are changed
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During El Nino years, the Trade Winds weaken and do not move warm water across the Pacific
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Storms develop in the middle of the Pacific bringing heavy winter rain to San Diego
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During El Nino, normally wet regions experience drought and wildfires
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Other areas, like S. California experience intense wave damage from storms
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Roads are destroyed and cliffs are eroded by waves and flooding
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Homes are flooded. Diseases spread by contaminated water.
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Accidents and injuries are greater with stormy weather
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Dry riverbeds in Arizona flood, damaging homes in Arizona
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Saturated hills slide, creating hazardous driving conditions
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Mudslides in on steep slopes destroy homes.
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Strong winds of El Nino knock down trees
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Ocean pier in S. California
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Buoys from San Diego’s Scripp’s Institute are stationed in the Pacific Ocean to monitor water temperature and El Nino events
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Density vs. Temperature It is the TEMP that is more important in stacking the layers of water Red (hot fresh) Clear (room temp fresh) Blue (cold salt) Yellow (warm salt)
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