SEDBIOL, a 1-D depth-resolving model, which couples physical, microbiologic
al, and sedimentation/resuspension submodels, is described. The physical su
bmodel uses a level 2 turbulence closure scheme forced by meteorology and t
idal elevations to provide seasonally varying turbulent diffusivites. Withi
n this framework is placed a model for water column microbiology, which inc
ludes the cycling of nitrogen and carbon through microplankton (phytoplankt
on and pelagic microheterotrophs) and detrital compartments. The microbiolo
gical system is closed by mesozooplankton grazing pressures taken from obse
rved zooplankton abundance. Inorganic and organic (microplankton and detrit
us) light-attenuating particulates sink through the water column depositing
at the seabed to form a superficial layer of 'fluff' from which they can b
e resuspended.
The model has been used to simulate conditions on the Goban Spur (49.5 degr
ees N 10.5 degrees W) in 200 m of water, using climatological meteorologica
l forcing, M2 tidal dynamics and zooplankton data from the Continuous Plank
ton Recorder (CPR) Survey. The results were compared with observed temperat
ure, chlorophyll, nitrate and annual primary production data taken as part
of the CEC MAST II Ocean Margin EXchange (OMEX) project, and with remotely
sensed chlorophyll. The physical submodel was calibrated against observed t
emperature profiles, and its fit improved by adding 'pseudo-weather' and a
relaxation term for deep-water temperature, and by increasing the value of
'background' eddy coefficients. The sensitivity of the microbiological mode
l to changes in the physical environment and several key parameters has bee
n tested, with values improved by fitting simulations to observed chlorophy
ll and nitrate concentrations. The coupled model was used to predict annual
net primary productivity, carbon fluxes into near-bed and fluff layers and
to compare the magnitude of biological and physical terms. (C) 2000 Elsevi
er Science B.V. All rights reserved.