Why equatorial counter current is not on equator?

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Why equatorial counter current is not on equator? Why it's not 4°S-4°N for example? What pushes it from equator in all 3 oceans?
"The Equatorial Counter Current is an eastward flowing, wind-driven current which extends to depths of 100–150 metres (330–490 ft) in the Atlantic, Indian, and Pacific Oceans. More often called the North Equatorial Countercurrent (NECC), this current flows west-to-east at about 3-10°N in the Atlantic, Indian Ocean and Pacific basins, between the North Equatorial Current (NEC) and the South Equatorial Current (SEC)"

Why it's not on equator? Why it's not 4°S-4°N for example? What pushes it from equator in all 3 oceans?

[Mentor Note -- Always provide attribution for quotes that you copy off the Internet; it is a copyright violation if you do not. Link added below]
https://en.wikipedia.org/wiki/Equatorial_Counter_Current
 
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  • #2
zasvitim said:
What pushes it from equator in all 3 oceans?
Ocean currents are driven by temperature and the salt concentration profile, that changes due to evaporation of water.

The continents obstruct, and the seafloor restricts, the ocean circulation.

Surface waves are driven by the wind, and that alternates with the seasons, between the Tropic of Cancer and of Capricorn, summer and winter, north and south, about ±23.5°

Click on a point to get current and wave height.
Open the "Earth" menu in the bottom left corner to select waves or atmosphere.
https://earth.nullschool.net/#curre...ht/winkel3=-358.89,-0.35,254/loc=-0.357,0.401
 
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  • #3
zasvitim said:
Why it's not on equator?
Because it's just a name. You may as well ask "Why does the Canary Current start around the Azores a thousand kilometres north-west of the Canary Islands?"
 
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1. Why is the Equatorial Counter Current not located exactly on the equator?

The Equatorial Counter Current is not located directly on the equator primarily due to the Coriolis effect, which influences the direction of wind and water flow. This effect causes ocean currents in the Northern Hemisphere to deflect to the right and those in the Southern Hemisphere to deflect to the left, creating a zone of weaker surface currents along the equator where the counter current can flow eastward against the prevailing trade winds.

2. What factors contribute to the formation of the Equatorial Counter Current?

Several factors contribute to the formation of the Equatorial Counter Current including the wind patterns, the Coriolis effect, and the distribution of oceanic heat. The trade winds blowing from east to west on either side of the equator pile up water in the western parts of the ocean basins, which then flows back eastward due to pressure gradients. This eastward flow is facilitated by the weaker Coriolis force at the equator, allowing the counter current to form between the north and south equatorial currents.

3. How does the Equatorial Counter Current differ from the surrounding currents?

The Equatorial Counter Current flows eastward, in contrast to the nearby North and South Equatorial Currents, which flow westward. This difference in direction is primarily due to the balancing act between pressure gradients and the Coriolis effect, which is minimal at the equator, allowing the counter current to flow opposite to the neighboring currents.

4. What role does the Equatorial Counter Current play in the global ocean circulation?

The Equatorial Counter Current plays a crucial role in redistributing heat and salt across the ocean basins, thereby aiding in the regulation of Earth's climate system. It helps in mixing the waters of the Atlantic, Pacific, and Indian Oceans, influencing global ocean circulation patterns and interconnecting different oceanic currents.

5. How does climate change impact the Equatorial Counter Current?

Climate change can impact the Equatorial Counter Current by altering wind patterns and ocean temperatures, which in turn can affect the strength and position of the current. Changes in global temperatures can lead to alterations in the trade winds and may modify the thermal structure of the oceans, potentially leading to variations in the behavior of the counter current and its influence on global climate.

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