Influence of the Atlantic Subpolar Gyre on the Thermohaline Circulation
Hjálmar Hátún, Anne Britt Sandø, Helge Drange, Bogi Hansen, Héðinn Valdimarsson
Abstract
Hjálmar Hátún, Anne Britt Sandø, Helge Drange, Bogi Hansen, Héðinn Valdimarsson
Abstract
During the past decade, record-high salinities have been observed in the Atlantic Inflow to the Nordic Seas and the Arctic Ocean, which feeds the North Atlantic thermohaline circulation (THC). This may counteract the observed long-term increase in freshwater supply to the area and tend to stabilize the North Atlantic THC. Here we show that the salinity of the Atlantic Inflow is tightly linked to the dynamics of the North Atlantic subpolar gyre circulation. Therefore, when assessing the future of the North Atlantic THC, it is essential that the dynamics of the subpolar gyre and its influence on the salinity are taken into account.
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During the past decade, record-high salinities have been observed in the Atlantic Inflow to the Nordic Seas and the Arctic Ocean, which feeds the North Atlantic thermohaline circulation (THC). This may counteract the observed long-term increase in freshwater supply to the area and tend to stabilize the North Atlantic THC. Here we show that the salinity of the Atlantic Inflow is tightly linked to the dynamics of the North Atlantic subpolar gyre circulation. Therefore, when assessing the future of the North Atlantic THC, it is essential that the dynamics of the subpolar gyre and its influence on the salinity are taken into account.
Key concepts: Ocean gyre, Thermohaline circulation, Oceanography, North Atlantic Deep Water, Shutdown of thermohaline circulation, Atlantic Equatorial mode, Atlantic multidecadal oscillation, Gulf Stream