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The MRCS is a coupling of the POLCOMS
baroclinic model with ERSEM,
a complex ecosystem model, on a 6 km grid set up in a pre-operational
system at the Met Office (Siddorn et al., submitted). Detailed
descriptions of the MRCS implementation of the POLCOMS are given
in Holt and James (2001) and Holt et al. (2004). It is a 3D baroclinic
finite difference model which uses an Arakawa-B grid in the horizontal
and hybrid S-coordinates in the vertical. This choice of grid,
the decision not to model explicitly the horizontal diffusion
and the use of a sophisticated horizontal advection scheme - the
Piecewise Parabolic Method (James, 1996) - combine to give the
model good frontal conserving properties.
The European Regional Seas Ecosystem Model (ERSEM) (Baretta et al.,
1995) was conceived as a generic model, and is one of the most complex
lower trophic-level marine ecosystem models currently in use. Its
philosophy is to include all those processes which significantly influence
ecosystem dynamics, and to resolve the ecosystem into sufficient functional
groups so that those processes can be sensibly defined. It thus has
one bacteria, four phytoplankton and three zooplankton functional
groups, and has a fully resolved diurnal cycle, variable carbon to
chlorophyll ratios and independent nutrient pools for carbon, nitrogen,
phosphorous and silicate. The inclusion of an 'over-wintering' physiology
for the mesozooplankton (Calanus-like) functional group has been included
to act as a proxy for the egg and early nauplii stages, overcoming
some of the problems associated with using the functional group based
approach for the more complex and behavioural life-stages of these
plankton. Coupled with this pelagic complexity is a benthic model,
designed to give not only detailed process information of the benthic
ecosystem (Ebenhöh et al., 1995), but also a well defined nutrient
coupling between the benthic and pelagic systems. Blackford et al.
(2004) give a full description of the ERSEM2004 model and parametrizations
used.
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Baretta, J.W., Ebenhöh, W. and Ruardij, P., 1995: The European
regional Seas Ecosystem Model, a complex marine ecosystem model. Netherlands
Journal of Sea Research, 33, 233-246.
Blackford, J.C., Allen, J.I. and Gilbert, F.J., 2004: Ecosystem dynamics
at six contrasting sites: A generic modelling study. Journal of Marine
Systems. 52, 191-215.
Ebenhöh, W., Kohlmeier C. and Radford, P.J., 1995: The benthic
biological model in the European Regional Seas Ecosystem Model. Netherlands
Journal of Sea Research, 38, 169-172.
Holt, J.T. and James, I.D., 2001: An s-coordinate density evolving
model of the northwest European continental shelf Part 1 model description
and density structure. Journal of Geophysical Research, 106, 14,015-14,034.
Holt, J.T., Proctor, R., Blackford, J.C., Allen, J.I. and Ashworth,
M., 2004: Advective controls on primary production in the stratified
western Irish Sea: an eddy-resolving model study. Journal of Geophysical
Research, 109, C05024.
James, I.D., 1996: Advection schemes for shelf sea models. Journal
of Marine Systems, 8, 237-254.
Siddorn, J.R., Allen, J.I., Blackford, J.C., Gilbert, F.J., Holt,
J.T., Holt, M.W., Osborne, J.P., Proctor, R. and Mills, D.K. (submitted).
Modelling the hydrodynamics and ecosystem of the north-west European
continental shelf for operational oceanography. Journal of Marine
Systems.
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