324
Chemical Oceanography, 4th Edition
3200
pCO 2
pCO
2 (µatm)
0.5
1.0
1.5
2.0
Ω
A
Ω A
2.5
3.0
3.5
4.0
2800
2400
Year
2000
1600
0
500
1000
1500
2000
2500
Figure 7.66
The expected change in the saturation state Ω over the next 1000 years. (From Millero, F.J., Woosley, R., DiTrolio,
B., and Waters, J., Oceanography, 22, 72–85, 2009. With permission.)
6
5
4
3
Calcification (% of preindustrial rate)
Ω A
2
1
0
0
20
40
60
80
100
120
140
2100 2065
1990 1880
Figure 7.67
The effect of the decrease in the saturation state of aragonite on the growth of corals. (Adapted from Langdon
and Atkinson, J. Geophys. Res. Oceans, 110, 1–16, 2005; Millero and DiTrolio, Elements, 6, 5, 299–303, 2010.)
Chemical Oceanography, 4th Edition
3200
pCO 2
pCO
2 (µatm)
0.5
1.0
1.5
2.0
Ω
A
Ω A
2.5
3.0
3.5
4.0
2800
2400
Year
2000
1600
0
500
1000
1500
2000
2500
Figure 7.66
The expected change in the saturation state Ω over the next 1000 years. (From Millero, F.J., Woosley, R., DiTrolio,
B., and Waters, J., Oceanography, 22, 72–85, 2009. With permission.)
6
5
4
3
Calcification (% of preindustrial rate)
Ω A
2
1
0
0
20
40
60
80
100
120
140
2100 2065
1990 1880
Figure 7.67
The effect of the decrease in the saturation state of aragonite on the growth of corals. (Adapted from Langdon
and Atkinson, J. Geophys. Res. Oceans, 110, 1–16, 2005; Millero and DiTrolio, Elements, 6, 5, 299–303, 2010.)