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Skip to Search Results- 2Deep Convection
- 2Labrador Sea
- 1Atlantic Meridional Overturning Circulation
- 1Buoyancy loss
- 1Eddies
- 1Finite element ocean model
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Fall 2021
The Labrador Sea experiences deep convection, a process where the oceans’ surface cools to the point where it may become more dense than the water at depth, promoting sinking and vertical mixing. This mixing can exceed 2000m in depth, producing a large volume of deep water, a crucial component in...
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Spring 2012
This thesis presents a modified version of the Finite Element Ocean Model (FEOM) developed at Alfred Wegener Institute for Polar and Marine Research (AWI) for the North Atlantic Ocean. A reasonable North Atlantic Ocean simulation is obtained against observational data sets in a Control simulation...