The currents that flow vertically in the ocean are called "upwelling" and "downwelling" currents. Upwelling occurs when deep, cold, nutrient-rich water rises to the surface, often supporting marine life. Downwelling, on the other hand, happens when surface water sinks due to density differences, often transporting oxygen-rich water to deeper layers. Both processes are crucial for ocean circulation and marine ecosystems.
These currents are called LongShore or Feeder Currents.
When electric currents are not allowed to flow, the circuit is called an open circuit. This means that there is a break in the circuit, preventing the flow of electricity from one point to another.
Materials that allow electrical currents to flow through them are called conductors. Examples of good conductors include metals such as copper, silver, and aluminum.
The mantle called the asthenosphere
Yes, the flow of water is CALLED a current.
currents that flow away
Vertically
The warm currents that flow from tropical areas are known as "warm ocean currents." These currents, such as the Gulf Stream in the Atlantic Ocean, transport warm water from the equator towards higher latitudes, influencing climate and weather patterns. They play a crucial role in regulating temperatures and supporting marine ecosystems in the regions they flow through.
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.
Currents that originate near the equator are called equatorial currents. These currents flow westward due to the trade winds and are typically warm. They play a significant role in regulating climate and oceanic circulation by redistributing heat across the globe. Equatorial currents are crucial for marine ecosystems and influence weather patterns in various regions.
In the southern hemisphere, ocean currents flow clockwise due to the Coriolis effect.