Two different eutrophication models as applied to the North Sea are di
scussed in this paper. The ERSEM (European Regional Seas Ecosystem Mod
el) model, being developed in the framework of the EU Marine Science a
nd Technology program, is a complex (70 state variables) ecosystem mod
el which dynamically simulates the large-scale cycling of carbon, oxyg
en and the macronutrients N, P and Si over the seasonal cycle. The mod
el consists of an interlinked set of modules, describing the biologica
l and chemical processes in the (stratified or non-stratified) water c
olumn and in the (vertically layered) benthic system, as forced by lig
ht and temperature. Advective and diffusive transport is included by d
riving the model with the output of the 3D General Circulation Model o
f the North Sea by Backhaus, aggregated into daily exchange volumes be
tween the ICES (International Council for the Exploration of the Sea)
boxes, which form the spatial compartments of the model. The other mod
el, MIKE21 EU, consists of an advanced 2D circulation model in combina
tion with modules describing advection-dispersion processes, oxygen dy
namics and carbon/nutrient cycling in the lower trophic levels. The ca
rbon and nutrient dynamics (N and P) are aggregated into 12 state vari
ables. The horizontal spatial resolution of the model is very high, wi
th a cell size of 18.5 x 18.5 km. Both models include the freshwater i
nflows and the associated organic and inorganic nutrient loadings as w
ell as cross-boundary flows as time series of flow rates and concentra
tions. The suitability of either model to address eutrophication-relat
ed questions is exemplified.