The region where deep open-ocean convection occurs in the Greenland Sea corresponds to that where a sea ice winter feature, the Odden, usually forms. The role of sea ice in modifying the surface waters to overturn to depth is evaluated through the combination of in siu measurements, satellite imagery, meteorological measurements and drifting buoy data. Results suggest local meteorological and oceanographic conditions govern the ice conditions over the region. The high ambient wave energy precludes the formation of ice beyond the frazil-pancake stage; the changing surface pressure field, due to passing storm systems, influences the daily shape and extent of the Odden and enables pancake ice to expel brine at an increased rate. Finally, the a...
The ocean response to air-sea flux variability in the Greenland Sea is investigated using a 1000 yea...
It is well known that warming of deep Atlantic Water in recent decades resulted in extensive retreat...
Water frequently coexists with ice on glaciers and ice sheets where water can be found under, within...
The region where deep open-ocean convection occurs in the Greenland Sea corresponds to that where a ...
The “Odden” is a large sea ice feature that forms in the east Greenland Sea that may protrude eastwa...
As part of the European Subpolar Ocean Programme (ESOP), the German research icebreaker Polarstern w...
The amount and spatial extent of Greenland Sea (GS) ice are primarily controlled by the sea ice expo...
The sensitivity of sea ice to the temperature of inflowing Atlantic water across the Greenland–Scotl...
The Odden ice tongue in the central Greenland Sea, believed to be associated with midgyre convection...
Hydrographic measurements from ships, autonomous profiling floats, and instrumented seals over the p...
This paper presents a statistical analysis of sea ice in the Greenland Sea (70-80N and 10W-10E) from...
This paper presents a statistical analysis of sea ice in the Greenland Sea (70-80N and 10W-10E) from...
Arctic sea ice loss continues to serve as a strong gauge of climate change. It is the component of t...
The extent and duration of sea ice in Baffi n Bay and Davis Strait has a major impact on the timing ...
The net annual sea ice volume exported through Fram Strait into the Greenland Sea amounts to about 1...
The ocean response to air-sea flux variability in the Greenland Sea is investigated using a 1000 yea...
It is well known that warming of deep Atlantic Water in recent decades resulted in extensive retreat...
Water frequently coexists with ice on glaciers and ice sheets where water can be found under, within...
The region where deep open-ocean convection occurs in the Greenland Sea corresponds to that where a ...
The “Odden” is a large sea ice feature that forms in the east Greenland Sea that may protrude eastwa...
As part of the European Subpolar Ocean Programme (ESOP), the German research icebreaker Polarstern w...
The amount and spatial extent of Greenland Sea (GS) ice are primarily controlled by the sea ice expo...
The sensitivity of sea ice to the temperature of inflowing Atlantic water across the Greenland–Scotl...
The Odden ice tongue in the central Greenland Sea, believed to be associated with midgyre convection...
Hydrographic measurements from ships, autonomous profiling floats, and instrumented seals over the p...
This paper presents a statistical analysis of sea ice in the Greenland Sea (70-80N and 10W-10E) from...
This paper presents a statistical analysis of sea ice in the Greenland Sea (70-80N and 10W-10E) from...
Arctic sea ice loss continues to serve as a strong gauge of climate change. It is the component of t...
The extent and duration of sea ice in Baffi n Bay and Davis Strait has a major impact on the timing ...
The net annual sea ice volume exported through Fram Strait into the Greenland Sea amounts to about 1...
The ocean response to air-sea flux variability in the Greenland Sea is investigated using a 1000 yea...
It is well known that warming of deep Atlantic Water in recent decades resulted in extensive retreat...
Water frequently coexists with ice on glaciers and ice sheets where water can be found under, within...