5 0
2 5
2 5
1
25
10
50
5 0
5
0
5 0
1
0
10
1 0 0
2 5
2 5
2 5
10
10
1 0
25
2
5
2 5
50
2 5
7
5
7 5
7 5
7
1
2
5
10
0
2 5 5 0
2 5
1 0
1 0
25
0°
90° E
90° W
180° W
30° N
60° N
POC export (gC m
−2 yr
−1 )
30° S
60° S
EQ
125
100
75
50
25
Ocean data view
0
Figure 8 Export production of particulate organic carbon (POC) from the inverse model. Redrawn from Schlitzer R (2000) Applying the adjoint method for global biogeochemical modeling.
In: Kasibhatla P, Heimann M, Rayner P, Mahowald N, Prinn RG, and Hartley DE (eds.) AGU Geophysical Monograph Series, Vol. 114: Inverse Methods in Global Biogeochemical Cycles,
pp. 107–124. Washington, DC: American Geophysical Union.
INVERSE MODELING OF TRACERS AND NUTRIENTS 197
2 5
2 5
1
25
10
50
5 0
5
0
5 0
1
0
10
1 0 0
2 5
2 5
2 5
10
10
1 0
25
2
5
2 5
50
2 5
7
5
7 5
7 5
7
1
2
5
10
0
2 5 5 0
2 5
1 0
1 0
25
0°
90° E
90° W
180° W
30° N
60° N
POC export (gC m
−2 yr
−1 )
30° S
60° S
EQ
125
100
75
50
25
Ocean data view
0
Figure 8 Export production of particulate organic carbon (POC) from the inverse model. Redrawn from Schlitzer R (2000) Applying the adjoint method for global biogeochemical modeling.
In: Kasibhatla P, Heimann M, Rayner P, Mahowald N, Prinn RG, and Hartley DE (eds.) AGU Geophysical Monograph Series, Vol. 114: Inverse Methods in Global Biogeochemical Cycles,
pp. 107–124. Washington, DC: American Geophysical Union.
INVERSE MODELING OF TRACERS AND NUTRIENTS 197