JEE Main Important Physics formulas
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Due to the rotation of the earth and its temperature, salinity and winds the water in oceans moves in a direction. This massive movement is known as Ocean currents. Ocean current is also the same as a river flow in oceans.
The ocean currents are mainly classified based on depth and temperature into four types, they are:
Surface currents
Deep currents
Warm currents
Cold currents
The movement of ocean currents, from warmer areas to colder areas. These ocean currents flow on the upper surface of the ocean. Hence it is known as the Surface ocean current.
Surface currents constitute about 10 per cent of all the water in the ocean.
These waters are in the top 400 metres of the ocean.
Deep waters sink into the deep ocean basins at high latitudes, where the ocean water flows from colder areas to warmer areas. These ocean currents flow from the deeper part of the ocean. Hence it is known as the Deeper ocean current.
The density rises as a result of the low temperatures.
The remaining 90% of the ocean's water is from deep water currents.
These waters move around the ocean basins due to variations in density and gravity.
Warm ocean currents bring warm water into cold-water areas.
These warm currents flow in large amounts away from the equatorial region.
They are usually observed on the east coast of continents in the low and middle latitudes (in both hemispheres).
They can be found on the west coasts of continents at high latitudes in the northern hemisphere.
Cold ocean currents bring cold water into warm water areas.
These cold waters in large amounts flow towards the equatorial region.
These currents are usually found on the west coast of the continents in the low and middle latitudes (in both hemispheres)
In the Northern Hemisphere; they observed on the east coast in the higher latitudes
Major ocean currents are greatly influenced by the stresses exerted through prevailing winds and Coriolis force.
The warm waters of lower latitudes move poleward, and the cold waters of the Arctic and Antarctic circles move towards warmer water in tropical and equatorial regions.
The oceanic circulation pattern roughly corresponds to the earth’s atmospheric circulation pattern. In higher latitudes, where the wind flow is mostly cyclonic, the oceanic circulation follows this pattern.
Due to the Coriolis force, the warm ocean currents from low latitudes tend to move to the right in the northern hemisphere and to their left in the southern hemisphere.
The oceanic circulation transports heat from one latitude belt to another in a manner similar to the heat transported by the general circulation of the atmosphere.
Ocean currents play a vital role in the Earth's climate system and the distribution of marine life. They also impact human activities such as shipping and fishing. Understanding the different types of ocean currents and how they function is essential for predicting weather patterns and climate changes, as well as for the management of marine resources. Further research on ocean currents is needed to better understand their complex interactions with the environment and to develop effective strategies for their conservation and sustainable use.
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