The Nordic Seas (Greenland, Iceland, and Norwegian Seas) are a site of open ocean convection that play an essential role in the Atlantic Meridional Overturning Circulation (AMOC), which profoundly affects surface heat transfer in the Northern Hemisphere, deep-ocean ventilation, and the global climate. Despite its global importance to Earth’s climate, the fate of open-ocean convection is still unresolved, especially regarding the potential effects of freshwater inputs from the demise of the Greenland ice sheet. While it is generally accepted that freshwater would drastically decrease the surface water density, thus preventing convection, there are still gaps in our understanding of the sensitivity of this system to freshwater input. By coupl...
Paleoceanographic changes of surface water characteristics have been studied in the Nordic Seas duri...
The modern rapidity of Arctic sea ice loss and rise in Arctic air and ocean temperatures is pushing ...
The ocean is an essential regulator of climate through its effect on redistribution of heat and air-...
Organisers; European Association of Geochemistry and of the Geochemical SocietySession 17h: Data and...
Surface waters in the Nordic Seas were colder and fresher throughout the marine isotope stage (MIS) ...
Orals Session CR1.2/CL4.09: Ice-sheet and climate interactions - paper no. EGU2017-6873In the North ...
Density changes in the upper water column of the northern North Atlantic may enhance or reduce verti...
Density changes in the upper water column of the northern North Atlantic may enhance or reduce verti...
Highlights • A thin mixed-layer and a strongly stratified upper-water characterized MIS 1. • ...
The Atlantic meridional overturning circulation (AMOC) is a critical element of Earth's climate syst...
In today's North Atlantic, warm and salty surface waters are transported northwards from the subtrop...
A striking characteristic of glacial climate in the North Atlantic region is the recurrence of abrup...
There is a growing body of evidence suggesting that the density and speed of the Nordic Seas overflo...
Sea surface temperature (SST) patterns in the northern North Atlantic, the Nordic seas, and the west...
Variable climatic and oceanographic conditions characterized the last interglacial at high northern ...
Paleoceanographic changes of surface water characteristics have been studied in the Nordic Seas duri...
The modern rapidity of Arctic sea ice loss and rise in Arctic air and ocean temperatures is pushing ...
The ocean is an essential regulator of climate through its effect on redistribution of heat and air-...
Organisers; European Association of Geochemistry and of the Geochemical SocietySession 17h: Data and...
Surface waters in the Nordic Seas were colder and fresher throughout the marine isotope stage (MIS) ...
Orals Session CR1.2/CL4.09: Ice-sheet and climate interactions - paper no. EGU2017-6873In the North ...
Density changes in the upper water column of the northern North Atlantic may enhance or reduce verti...
Density changes in the upper water column of the northern North Atlantic may enhance or reduce verti...
Highlights • A thin mixed-layer and a strongly stratified upper-water characterized MIS 1. • ...
The Atlantic meridional overturning circulation (AMOC) is a critical element of Earth's climate syst...
In today's North Atlantic, warm and salty surface waters are transported northwards from the subtrop...
A striking characteristic of glacial climate in the North Atlantic region is the recurrence of abrup...
There is a growing body of evidence suggesting that the density and speed of the Nordic Seas overflo...
Sea surface temperature (SST) patterns in the northern North Atlantic, the Nordic seas, and the west...
Variable climatic and oceanographic conditions characterized the last interglacial at high northern ...
Paleoceanographic changes of surface water characteristics have been studied in the Nordic Seas duri...
The modern rapidity of Arctic sea ice loss and rise in Arctic air and ocean temperatures is pushing ...
The ocean is an essential regulator of climate through its effect on redistribution of heat and air-...