PISCES biogeochemical model - NEMO
PISCES biogeochemical model - NEMO
PISCES biogeochemical model - NEMO
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Figure 1: Architecture of <strong>PISCES</strong>. This figure only shows the ecosystem <strong>model</strong> omitting thus<br />
oxygen and the carbonate system. The element which are explicitely <strong>model</strong>ed are indicated in<br />
the left corner of each box.<br />
except for the silicon, chlorophyll and iron content of phytoplankton. Finally, all parameters<br />
and their standard values in <strong>PISCES</strong> are listed in Table 1 at the end of this section.<br />
3.1 Equation for nanophytoplankton<br />
∂P<br />
∂t = (1 − δnano )µ nano P − m nano P<br />
K nano + P P − wnano p P 2 − g micro (P )Z − g micro (P )M (1)<br />
The production terms for nano/picophytoplankton is defined by :<br />
µ nano = µ P<br />
⎛<br />
⎝1 − e<br />
α P ( Chl<br />
C<br />
)P P AR<br />
µ P L nano<br />
lim<br />
⎞<br />
⎠ L nano<br />
lim (2)<br />
where µ P = ab cT and where the limitations terms are defined as follows:<br />
L nano<br />
po4 =<br />
L nano<br />
fe =<br />
L nano<br />
no3 =<br />
P O 4<br />
Kpo4 nano + P O 4<br />
F e<br />
K nano<br />
F e<br />
+ F e<br />
Kno3<br />
nano Knh4<br />
nano<br />
K nano<br />
nh4 NO 3<br />
+ K nano<br />
nh4<br />
NO 3 + K nano<br />
no3 NH 4<br />
3