The warm, low salinity waters from Pacific are transported into Indian ocean's South Equatorial Current.
Most counter currents near the equator flow westward, in the opposite direction to the predominant eastward-flowing equatorial currents, such as the Equatorial Undercurrent. These counter currents help redistribute heat and nutrients in the ocean and play a crucial role in the global climate system.
The North Equatorial Current and South Equatorial Current in the Pacific Ocean are both warm, fast-moving currents that flow towards the west. They are driven by the trade winds. One key difference is that the North Equatorial Current is influenced by the North Pacific Gyre, while the South Equatorial Current is influenced by the South Pacific Gyre.
Ocean currents flow from east to west near the sub-equatorial area. These winds are called "trade winds" and they start in Portugal, they move to the Canary Islands, to the Cape Verde and then to the West part of the Caribbean.
The Trade Winds are responsible for the westward flow of equatorial currents due to their consistent easterly direction, blowing from the subtropical high-pressure areas toward the equator. This wind pattern pushes surface water westward across the equatorial regions, contributing to the creation of currents like the North and South Equatorial Currents. Additionally, as these winds drive the surface water, they influence the overall oceanic circulation, reinforcing the westward flow. Thus, the Trade Winds play a crucial role in shaping ocean currents in the tropics.
An equatorial cir, or equatorial current, refers to the ocean currents that flow along the equator in both the Atlantic and Pacific Oceans. These currents are primarily driven by trade winds and play a crucial role in regulating global climate by distributing heat across the planet. They also influence marine ecosystems and navigation patterns for ships. The equatorial current system includes features like the North and South Equatorial Currents, which help facilitate the larger ocean circulation patterns.
North Equatorial flow clockwise and southern counter-clockwise.
Ocean and wind currents above the equator flow in a clockwise pattern, while those south of the equator flow in a counterclockwise pattern. But all the winds and currents meet at the equator and flow east to west forming the trade winds and equatorial currents.
In the ocean floor.
Ocean currents flow near the equator from the east to west. Ocean currents flow near the poles from west to east.
On the average, it most often blow horizontally.
The Current in the ocean spins in a circle.
Ocean currents flow near the equator from the east to west. Ocean currents flow near the poles from west to east.