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Oceans and Climate Changes
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Movement of water from one place to another
Ocean Currents Movement of water from one place to another
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Surface Currents Powered by wind Move upper few 100 meters of seawater
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Wind forms when air in an area of high pressure moves to an area of lower pressure
Equator’s warm air is pushed up by denser, colder air The Pole’s cold air, sinks below less dense air
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Due to the movement of the earth, wind and currents DO NOT move in straight lines
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The Coriolis Effect – rotation of the Earth causes moving air and water to change direction
To the right north of the equator To the left south of the equator
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Gulf Stream Current - Warm
Atlantic Ocean Brings warm water from the equator up North Keeps N. American East Coast Waters warm Keeps Iceland mild and ice-free all year
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California Current - Cold
Pacific Ocean Brings waters from North pole down South Keeps North American West Coast Cool
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Density Currents More dense water sinks and pushes up less dense water
This moves water around globe
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What makes Water Dense? Cold Temperature
High Salinity (amount of salt in water)
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Cold, Salty Water When water freezes, salts are dissolved and left in unfrozen water This makes unfrozen water VERY DENSE When frozen water melts, it is less dense This causes a change in density and movement of water…DENSITY CURRENTS
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WHY IS THIS IMPORTANT?
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It is important because…
If the ice caps where to melt, then we would have a large amount of less dense water If salinity is reduced, then density currents would WEAKEN or STOP This would cause major CLIMATE SHIFTS Change in climate Change in weather
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El Nino An occasional climatic event in which strong Pacific winds WEAKEN or REVERSE
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Effects of El Nino Ocean temperatures near Peru HEAT UP.
The position and strength of one of the jet streams may be altered, changing wind and precipitation patterns around the world. Africa and Australia may experience drought
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The winds blowing across the Pacific are stronger than normal
La Nina The winds blowing across the Pacific are stronger than normal
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