‚an Leeuwen et al.
10.3389/fmars.2023.1129951
5 HS
5
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N:P ratio
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nl netPP
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a
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Longitude [deg. E]
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„ongitude [deg. E17
nn
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>
cs
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Difference
(
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D
Er
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OS
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
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RBINS
SMHI
UHH-HZG)
Of
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5 40 60
Winter Total N, depth-averaged (CS, umolL
300
250
E
200%.
sn
an
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7
514]
21.4
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GC
Pre-eutrophic state
hm kl Ch
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PMZ PM
MM
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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