Upload
elizabeth-walters
View
217
Download
3
Tags:
Embed Size (px)
Citation preview
Surface Currents
1. Caused by friction between the ocean and the wind that blows across its surface
2.Created by the prevailing wind system
3. Currents are closely related to the general circulation pattern of the atmosphere
4. Can be localized, seasonal or permanent
The major cause of gyres is…
•the Coriolis effect – the deflection of currents away from their original as a result of the Earth’s rotation
Northern Hemisphere – deflection to the right
Southern Hemisphere – deflection to the left
Currents and Climate low latitude currents move to high
latitudes – transferring heat from the warm to the cooler areas
High latitude currents move to low latitudes – transferring cooler water to warmer climates
Ocean water movement accounts for ¼ of heat transport on the Earth
•The Gulf Stream brings warmer water to Great Britain and Northwestern Europe
•Causes warmer winters (felt in the middle latitudes)
Upwelling Wind induced
▫The vertical rising of cooler water from deeper layers of the ocean to replace warmer surface water
▫cooler temperatures brings greater amounts of nutrients and therefore greater amount of fish and other marine life
Deep Ocean Circulation•Significant vertical movement
▫Accounts for the thorough mixing of deep- water masses
Density Currents•Dense water sinks and spreads out beneath the ocean’s surface
•Increased density caused by: decrease in temperature increase in salinity
High Latitudes (decrease in temps.)
where most deep currents begin sea-ice is formed due to cold temps., leaving behind a greater salinity of remaining water, which then sinks
highest density of ocean water found near Antarctica
ocean water sinks and travels the ocean basin for some 500-2000 years
Evaporation (increases in salinity)
high temps. - increase evaporation
less water leads to greater salinity of remaining water
remaining water sinks to ocean basin and travels the globe
Conveyor Belt – Thermohaline Circulation
warm surface water flows towards the poles
at the poles water temp. drop - salinity increases making it more dense and it sinks
sinking water then moves towards the equator on the ocean floor
at the equator the water is cold and deep
deep water eventually upwells to complete the circuit –
• influences global climate by warm water releasing heat into the atmosphere