09.01.2015 Views

PISCES biogeochemical model - NEMO

PISCES biogeochemical model - NEMO

PISCES biogeochemical model - NEMO

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

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

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!