Equatorial Undercurrent is a subsurface current flowing eastward along the equator. A narrow, swift-flowing ribbon with a thickness of 200 m and a width of at most 400 km, it displays the largest current speeds of the equatorial current system.
The Pacific Equatorial Undercurrent is also known as the Equatorial Undercurrent. It is a narrow, deep, and swift eastward-flowing ocean current located in the equatorial region of the Pacific Ocean.
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.
North Equatorial flow clockwise and southern counter-clockwise.
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.
westward
undercurrent of room was cold
Undercurrent is a noun.
The Undercurrent was created on 2007-04-02.
The trade winds, which blow predominantly from east to west in the tropics, exert a significant force on the surface of the ocean. This wind-driven movement pushes water westward across the equatorial region, creating the equatorial currents. Additionally, the Coriolis effect causes the water to veer slightly to the right in the Northern Hemisphere and to the left in the Southern Hemisphere, but the dominant flow remains westward due to the consistent direction of the trade winds. As a result, these winds play a crucial role in establishing and maintaining the westward flow of the equatorial current.
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.
Sophie Wacongne has written: 'Dynamics of the equatorial undercurrent and its termination' -- subject(s): Ocean currents, Thermoclines (Oceanography), Ocean circulation, Mathematical models
Winds are named for the direction they flow from. For example, a northeast wind comes from the northeast direction.