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Skip to Search Results- 2Labrador Sea
- 2Labrador Sea Water
- 1Atlantic Meridional Overturning Circulation
- 1Buoyancy loss
- 1Deep Convection
- 1Freshwater
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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 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...