Ocean currents flow near the equator from the east to west. Ocean currents flow near the poles from west to east.
Ocean currents flow near the equator from the east to west. Ocean currents flow near the poles from west to east.
Surface currents near the equator typically flow east to west, driven by the trade winds. Near the poles, surface currents flow from west to east, driven by the westerlies. The Coriolis effect influences the direction of surface currents in both regions.
westward
On the average, it most often blow horizontally.
The wind that drives equatorial currents is primarily the Trade Winds. These winds blow consistently from east to west near the equator, pushing surface waters in the same direction and creating equatorial currents. The Coriolis effect also influences the direction of these currents.
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.
Equator due to the trade winds pushing the surface waters westward. This creates the Equatorial Counter Current, which flows eastward at the surface.
The curved paths of global winds and surface currents are caused by warm air near the equator.
near the equator
As the equator is warm, the currents that originate from there are also warm.
Stream like movements of water at tor near the surface of the ocean are called currents. A current's direction and strength is influenced by depth contours, shoreline configurations and interaction with other currents.
Stream like movements of water at tor near the surface of the ocean are called currents. A current's direction and strength is influenced by depth contours, shoreline configurations and interaction with other currents.