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Skip to Search Results- 6Labrador Sea
- 2Deep Convection
- 2Labrador Sea Water
- 1Arctic
- 1Atlantic
- 1Atlantic Meridional Overturning Circulation
- 1Galbraith, Eric D. (Experimental Sciences & Mathematics, UAB)
- 1Myears, Paul G. (Department of Earth and Atmospheric Sciences)
- 1Myers, Paul (Earth and Atmospheric Sciences)
- 1Myers, Paul G. (Department of Earth and Atmospheric Sciences, U of A)
- 1Myers, Paul G. (Earth and Atmospheric Sciences)
- 1Paul G. Myers (Department of Earth and Atmospheric Sciences)
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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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Fall 2018
The Arctic and the North Atlantic Oceans are experiencing multiple stresses such as loss of sea ice, changing atmospheric patterns, increasing wind energy at the ocean surface and larger freshwater discharge to coastal regions. To address how the marine system may respond to these stresses I...
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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...
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Fall 2019
The rising concentration of anthropogenic heat-trapping gasses has resulted in an energy imbalance in the Earth's climate system. As a consequence of it, an enhanced hydrological cycle and the continuous decline of the ice sheets are expected to increase the freshwater input into the Arctic and...
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The Effects of Tides and Submesoscale Mixed Layer Eddies on Deep Convection in the Labrador Sea: Simulations at Resolutions Consistent with Coupled Climate Models
DownloadFall 2024
The Intergovernmental Panel on Climate Change predicts that the large-scale overturning circulation will weaken over the 21st century. As with many other oceanic consequences of anthropogenic climate forcing, such as increased warming, acidification, glacial and sea ice melt, marine heatwaves,...