Conveyor Belt Cycling describes the movement of the ocean water between surface and deep water.
Deep currents
The water that forms far below the surface is called a Deep Current.
The movement of deep cold and nutrient-rich water to the surface is known as upwelling. Upwelling occurs when winds push surface water away from a coastline, causing the deep colder water to rise and replace it. This process brings up essential nutrients from the deep ocean to the surface, supporting the growth of phytoplankton and other marine life.
Ocean currents
Deep current is a movement of the ocean water. The ocean waters current is continuous.
Ocean convection currents move the deep cold water to the surface of oceans.
An upwelling is a current in the ocean that brings deep, cold water to the ocean surface.
deep currents streamlike movement of water that flow very slowly along the ocean floor. surface current can influence the climate of land are they flow past.
Deep currents are streamlike movements of water that flow very slowly along the ocean floor. Deep currents occur when the cold, dense water from the poles sinks below warmer, less sense ocean water and flows towards the equator.
gulfstream
Well, honey, a surface current is like the diva strutting her stuff on the runway - it's the flashy, visible movement of water caused by things like wind and tides. On the other hand, a deep current is more like the mysterious loner lurking in the shadows - it's the slow, hidden flow of water deep below the surface, driven by differences in temperature and salinity. So, in a nutshell, surface currents are the show-offs, while deep currents are the silent movers and shakers of the ocean.
The movement of deep water in the ocean basins is by density driven forces and gravity.