“…To estimate POP export to the deeper ocean beyond the shelf edge, we combined transport fields from the high resolution prognostic model setup for the coupled North Sea and Baltic Sea (lateral boundary at 60 • N) [23] with results from an exterior diagnostic shelf sea model [34]. The horizontal resolution of the advection model was ∆ϕ = 6 and ∆λ = 10 , and in the vertical, the water column was resolved by 20 z-levels with the lower boundaries at 5,10,15,20,25,30,35,40,48,56,64,72,80,88,100,125,150,200, 400 and 3500 m. The hydrodynamic model setup has previously underwent extensive validations [35], and it has been shown to well-replicate the interannual variations in the hydrodynamic conditions in the North Sea and Baltic Sea system [36]. From a long term ECOSMO model simulation [28] that was forced by atmospheric boundary conditions from the NCEP/NCAR re-analysis [37], we selected the years 2004-2008, for which we had atmospheric inputs and high resolution river load data available.…”