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Full text: Deriving pre-eutrophic conditions from an ensemblemodel approach for the North-West European seas

‚an Leeuwen et al. 
10.3389/fmars.2023.1129951 
5 HS 
5 
En 
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N:P ratio 
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Gut 
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Longitude [deg. E] 
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La X 
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Sal 
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s 
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> u 5 
„ongitude [deg. E17 
nn 
1s 
> 
cs 
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Difference 
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DD 
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10 
=; U 
! onaitude [deag. E1 
:IGURE 10 
difference between the ensemble results (unweighted) for the current state (CS) and the pre-eutrophic state (historic scenario, HS) for the N:P ratio 
‘'A), net primary production (B) and near bed oxygen levels (C). Green colours indicate areas where the pre-eutrophic levels were lower than those 
3f the current state. Note the changing colour bar scale, for O» the scale starts at 1%. 
zedfield 
ao 
Current state 
8 SCHPMI v MPM 
61 
4 
4 SCHPM2 
3 MPM 
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MM 
Ad 
SD 
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ACH 
* Deltares 
» IFREMER | 
JRC 
Oktenburg! 
RBINS 
SMHI 
UHH-HZG) 
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C3 
5 40 60 
Winter Total N, depth-averaged (CS, umolL 
300 
250 
E 
200%. 
sn 
an 
16} 
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514] 
21.4 
N 
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GC 
Pre-eutrophic state 
hm kl Ch 
SCHPM1 
PMZ PM 
MM 
RACE 
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> RBINS 
SMHI 
> UHH-HzG| 
“ BAM co 
Winter Total N, depth-averaged (HS, umol L 
30 
N 
{ 
300 
250 
IC 
50 
AUGURE 11 
Model results of winter total phosphorus concentration (Ptot) as a function of winter total nitrogen concentration (Ntot) in each area for each 
model. (A) current conditions, (B) pre-eutrophic conditions (both 2009-2014). The colours indicate the modelled net primary production (NPP) for 
:he corresponding areas and models. The line indicates the global ocean Redfield ratio (N:P = 16). Only some outlying results have been named, for 
area acronyms see Appendix C. 
"rontiers in Marine Science 
frontiersin.org
	        
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