Hydrographic changes in the Labrador Sea, 1960–2005¶
Yashayaev. (2007). Hydrographic changes in the Labrador Sea, 1960–2005.
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Domain-specific¶
- Downwelling
- Each winter, cold, dry air over the subpolar North Atlantic strips heat from the surface ocean; the chilled surface water grows denser than the layers beneath it, and once that density contrast overturns the stratification, the water column convects — surface water plunges in narrow plumes to roughly 1,500–2,000 m, forming Labrador Sea Water
This sourceFour-decade hydrographic record of the Labrador Sea documenting Labrador Sea Water formation and the strong interannual range of convection depth, from a few hundred metres in stratified years to beyond 2,000 m in the deepest early-1990s winters.
- Each winter, cold, dry air over the subpolar North Atlantic strips heat from the surface ocean; the chilled surface water grows denser than the layers beneath it, and once that density contrast overturns the stratification, the water column convects — surface water plunges in narrow plumes to roughly 1,500–2,000 m, forming Labrador Sea Water
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