File:Figure 5.25 - Predicted aragonite saturation state of the surface ocean in the year 2100.png

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Figure_5.25_-_Predicted_aragonite_saturation_state_of_the_surface_ocean_in_the_year_2100.png(645 × 276 pixels, file size: 136 KB, MIME type: image/png)

Predicted aragonite saturation state of the surface ocean in the year 2100 (Orr et al., 2005[1]). The dashed line represents the saturation horizon and shows that much of the Southern Ocean (<50ºS) is expected to be under-saturated with respect to aragonite by 2100.

  1. Orr, J.C., Fabry, V.J., Aumont, O., Bopp, L., Doney, S.C., Feely, R. A., Gnanadesikan, A., Gruber, N., Ishida, A., Joos, F., Key, R.M., Lindsay, K., Maier-Reimer, E., Matear, R., Monfray, P., Mouchet, A., Najjar, R.G., Plattner, G.K., Rodgers, K.B., Sabine, C.L., Sarmiento, J.L., Schlitzer, R., Slater, R.D., Totterdell, I.J., Weirig, M.F., Yamanaka, Y. and Yool, A. 2005. Anthropogenic ocean acidification over the twenty-first century and its impact on calcifying organisms, Nature, 437, 681-686.

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