NORTH EQUATORIAL CURRENT Meaning and
Definition
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The North Equatorial Current is a major oceanic current that forms part of the global system of tropical currents. It is a warm ocean current that flows in an east-to-west direction near the equator in the Pacific Ocean. The current originates from the eastern side of the Pacific Ocean, near the coast of Central America, where the trade winds blow from east to west. As these trade winds push the surface waters of the ocean, they result in the formation of the North Equatorial Current.
This current is characterized by its relatively high temperature and weak currents. It typically flows at speeds ranging from 5 to 10 centimeters per second. As it moves westward, it splits into different branches, with some portions of the current eventually merging with the warm waters of the West Wind Drift in the Western Pacific.
The North Equatorial Current plays a significant role in the climate and weather patterns of the regions it passes through. It helps distribute heat and energy from the tropical regions towards the mid-latitudes. It also influences the distribution of marine life, as it serves as a transportation mechanism for various planktonic organisms and larvae of marine species.
In summary, the North Equatorial Current is a warm oceanic current that flows east to west near the equator in the Pacific Ocean. It is influenced by the trade winds, and its role in heat distribution and marine life transportation makes it a crucial component of the global oceanic circulation system.
Common Misspellings for NORTH EQUATORIAL CURRENT
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