CHAPTER 1 . The Carbonate System in Marine Environments
340
320
E
1;;
.a- 300
l
280
260
0
380
360
i
340
.aN
8
Q.
320
300
280
14
380
360
I
l340
320
0
0
16
18
34.8
35.0
35.2
0
2
Chlorophyl l {jJg 1-1}
20
22
Temperature {oG
35.4
Salinity
35.6
23
3
4
24
26
35.8
36.0
Fig. 1.9. The relationship between the partial pressure of carbon dioxide in Atlantic surface waters to
the concentrations of chlorophyll, temperature and salinity (Millero 1996)