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A Simple Ice–Ocean Model for the Greenland Sea
East Greenland Current Greenland Sea Ice–Ocean Model
2009/1/5
A steady, coupled model of the upper ocean circulation and ice cover in a meridional channel is presented and applied to the Greenland Sea. The main ocean gyre is driven by wind stress; however a nonz...
A Simple Steady-State Coupled Ice-Ocean Model, with Application to the Greenland-Norwegian Sea
A Simple Steady-State Greenland-Norwegian Sea Ice-Ocean Model
2008/12/30
A thermodynamic reduced-gravity ocean model forced by the steady-state surface wind stress and a Haney-type heat flux was used to determine the climatological ice-edge position, ice thickness, ocean c...
Numerical Investigation of the Circulation In the Greenland and Norwegian Seas
Numerical Investigation Norwegian Seas Greenland
2008/12/23
An ocean general circulation model is used to investigate the circulation in the Greenland and Norwegian seas. The primitive equations are solved on 12 levels with a horizontal grid-point distance of ...
Three-Dimensional Observations of a Deep Convective Chimney in the Greenland Sea during Winter 1988/89
turbulent kinetic energy Arctic Intermediate Water Deep Convective Chimney Greenland Sea
2008/12/11
All available temperature data, including moored thermistor, hydrographic, and tomographic measurements, have been combined using least-squares inverse methods to study the evolution of the three-dime...
Circulation and Fluxes in the North Atlantic between Greenland and Ireland
East Greenland Current Circulation Fluxes Ireland
2008/11/24
Quasi-meridional flux estimates for volume, heat, and freshwater, with computed errors, in the region of the subpolar gyre of the North Atlantic between Cape Farewell and Ireland between 53° and 60°N ...
An Investigation of the Dynamics of the East Greenland Current in Fram Strait Based on a Simple Analytical Model
East Greenland Current Fram Strait Simple Analytical Model
2008/7/21
The East Greenland Current (EGC) in Fram Strait is examined in summer, based on the hydrographic data from the MIZEX 84 experiment, and its dynamics is further analyzed using a simple analytical model...
Is Bottom Boundary Layer Mixing Slowly Ventilating Greenland Sea Deep Water
Bottom Boundary Layer Greenland Sea Deep Water
2008/6/26
Bottom water temperatures in the central Greenland Sea have been increasing for the last two decades. The warming is most likely related to the absence of deep convective mixing, which cools and fresh...