This numerical simulation is based on MITgcm and uses a setup of Nguyen et al. (2011). 
The initial conditions are from WOA09; the boundary conditions are provided by an ECCO2
optimized global solution (cube92); the model is forced by JRA25 winds and fluxes.

deltaT = 300
dimensions [1680 1536]

For detailed information on the model setup and parameters of this experiment see data* files
in 'setup' folder.

When using this model output please site:

Volkov D.L., A.A. Kubryakov, R. Lumpkin (2015), Formation and variability of the Lofoten Basin
vortex in a high-resoltuion ocean model, Deep-Sea Res. Part I.

Nguyen, A.T., D. Menemenlis, and R. Kwok (2011), Arctic ice-ocean simulation with optimized model
parameters: approach and assessmnet, J. Geophys. Res., 116, C04025, doi:10.1029/2010JC006573.