30
§
..r::
a CII
0
2000
O~~~.---,----,----,---~
2100
2200
2300
2400
2500
1000
2000
North
Atlantic
3000
4000
5000
F. J. Millero
Fig. 1.17. Depth profile of the normalized total carbon dioxide (NTC02) in the Atlantic and Pacific oceans
(Millero 1996)
2000
§
..r:: ... Do CII
0
4000
6000 - - - - -
40S
30
20
10
EO
10
20
30N
Fig. 1.18. A section of NTC02 in the Atlantic Ocean (Millero 1996)
This value is about 14 for cold waters and 8 for warmer waters (the average is about 10 ).
Thus, a 10% change in Pco 2 results in only a 1% change in Te02• This factor is important when considering the effect that increases of CO2 in the atmosphere have on the
carbonate system.
§
..r::
a CII
0
2000
O~~~.---,----,----,---~
2100
2200
2300
2400
2500
1000
2000
North
Atlantic
3000
4000
5000
F. J. Millero
Fig. 1.17. Depth profile of the normalized total carbon dioxide (NTC02) in the Atlantic and Pacific oceans
(Millero 1996)
2000
§
..r:: ... Do CII
0
4000
6000 - - - - -
40S
30
20
10
EO
10
20
30N
Fig. 1.18. A section of NTC02 in the Atlantic Ocean (Millero 1996)
This value is about 14 for cold waters and 8 for warmer waters (the average is about 10 ).
Thus, a 10% change in Pco 2 results in only a 1% change in Te02• This factor is important when considering the effect that increases of CO2 in the atmosphere have on the
carbonate system.