Upwelling

//Upwelling// can be [|described] as the natural occurance of bottom dwelling nutrients floating up to the surface or the movement of cold, dense water to the much less dense surface. //Upwelling// is also related to the development of certain species of fish, such as sardines.

There are five specific types of //Upwelling//:


 * __Coastal Upwelling__**-The water along continental coasts is heated by the sun during the summer which causes Temperature Stratification. Strong winds, usually originating in the Gulf of Mexico, combined with the earth's Coriolis Force or Effect result in the cold water on the bottom of the ocean to rise to the surface, usually bringing nutrients with it.


 * __Large Scale Wind Driven Upwelling__**-Upwelling greatly influence by winds. You may see Large Scale Wind Driven Upwelling when researching Australian coastal geography.

The lesser known forms of Upwelling are known as:
 * __Eddie Associated Upwelling

Topographically-Associated Upwelling

Broad Diffusive Upwelling__**

Other Topics of Interest: //Water Pessure//, //Overfishing

< // Bibliography>

"Upwelling." //Amazines: Free Articles and Web Content//. Web.

"Coastal Upwelling." //The Cool Room//. Web.

"Coastal Upwelling." //Northwestern Fisheries Science Center//. Web.

"Upwelling." //WW2010 University of Illinois//. Web.

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