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Upwelling is a process by which cold water is brought up from the depths of the ocean.
The thermohaline circulation is a term for the global density-driven circulation of the oceans. Derivation is from thermo- for heat and -haline for salt, which together determine the density of sea water
Deep ocean circulation(90% of ocean water) is caused by differences in temperature, salinity and suspended load. It is referred to as "Thermohaline"- meaning heat and salt- circulation.
Thermohaline circulation brings oxygen rich water to the deep ocean.
Heat
Upwelling is caused by currents on the surface. When water moves from the bottom of the ocean towards the surface it is called upwelling. Downwelling is when more dense water sinks. This process moves nutrients back to the deep part of the ocean.
Upwelling
Upwelling is water raising from deep in the ocean to the surface. It can be caused by wind ar density currents.
how does upwelling bring fish and nutrients to the surface
An upwelling is a current in the ocean that brings deep, cold water to the ocean surface.
Upwelling
Upwelling is a process by which cold water is brought up from the depths of the ocean.
Rises to the surface.
Global Conveyor Belt
Conveyor Belt Cycling describes the movement of the ocean water between surface and deep water.
The water brought to the surface by upwelling tends to be richer in nutrients than the water it replaces--more nutrients, more life.
Upwelling is when the winds cause nutrient rich waters from lower levels of the ocean to replace the surface water. Upwelling's are usually caused by coastal surges or open oceans.