Figures and Tables
From the following article:
James C. Orr, Victoria J. Fabry, Olivier Aumont, Laurent Bopp, Scott C. Doney, Richard A. Feely, Anand Gnanadesikan, Nicolas Gruber, Akio Ishida, Fortunat Joos, Robert M. Key, Keith Lindsay, Ernst Maier-Reimer, Richard Matear, Patrick Monfray, Anne Mouchet, Raymond G. Najjar, Gian-Kasper Plattner, Keith B. Rodgers, Christopher L. Sabine, Jorge L. Sarmiento, Reiner Schlitzer, Richard D. Slater, Ian J. Totterdell, Marie-France Weirig, Yasuhiro Yamanaka & Andrew Yool
Nature 437, 681-686(29 September 2005)
doi:10.1038/nature04095
Figure 1
Increasing atmospheric CO2 and decreasing surface ocean pH and [CO32-].
Full size figure and legend (85K)Figure 2
The aragonite saturation state in the year 2100 as indicated by
[CO32-]A.
Figure 4
Key surface carbonate chemistry variables as a function of pCO2.
Full size figure and legend (45K)Figure 5
Average surface [CO32-] in the Southern Ocean under various scenarios.
Full size figure and legend (48K)





