The functionality of biogeochemical models in GOTM is demonstrated here for
four different scenarios:
- The idealised channel flow scenario introduced in
section 12.1.2 is here complemented with a simple suspended matter
equation, see section 12.5.1.
- The PROVESS Northern North Sea scenario (see section 12.2.2)
is here coupled to the NPZD model, see section 12.5.2.
- The Fladenground Experiment (FLEX'76), see section 12.2.1
is here coupled to the Fasham et al. (1990) biogeochemical model,
see section 12.5.3.
- The multiannual Gotland Deep scenario (see section 12.2.5)
coupled to the biogeochemical model by Neumann et al. (2002),
with adaptations by Burchard et al. (2006), see section 12.5.4.