Journal cover Journal topic
Biogeosciences An interactive open-access journal of the European Geosciences Union
Biogeosciences, 7, 979-1005, 2010
© Author(s) 2010. This work is distributed
under the Creative Commons Attribution 3.0 License.
11 Mar 2010
Projected 21st century decrease in marine productivity: a multi-model analysis
M. Steinacher1,2, F. Joos1,2, T. L. Frölicher1,2, L. Bopp3, P. Cadule3, V. Cocco1,2, S. C. Doney4, M. Gehlen3, K. Lindsay5, J. K. Moore6, B. Schneider7, and J. Segschneider8 1Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
2Oeschger Centre for Climate Change Research, University of Bern, Zähringerstrasse 25, 3012 Bern, Switzerland
3Laboratoire du Climat et de l'Environnement (LSCE), L'Orme des Merisiers Bât. 712, 91191 Gif sur Yvette, France
4Dept. of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA
5Climate and Global Dynamics Division, National Center for Atmospheric Research, Boulder, CO 80307, USA
6Dept. of Earth System Science, University of California, Irvine, CA 92697, USA
7Institute of Geosciences, University of Kiel, Ludewig-Meyn-Str. 10, 24098 Kiel, Germany
8Max-Planck-Institut für Meteorologie, Bundesstrasse 53, 20146 Hamburg, Germany
Abstract. Changes in marine net primary productivity (PP) and export of particulate organic carbon (EP) are projected over the 21st century with four global coupled carbon cycle-climate models. These include representations of marine ecosystems and the carbon cycle of different structure and complexity. All four models show a decrease in global mean PP and EP between 2 and 20% by 2100 relative to preindustrial conditions, for the SRES A2 emission scenario. Two different regimes for productivity changes are consistently identified in all models. The first chain of mechanisms is dominant in the low- and mid-latitude ocean and in the North Atlantic: reduced input of macro-nutrients into the euphotic zone related to enhanced stratification, reduced mixed layer depth, and slowed circulation causes a decrease in macro-nutrient concentrations and in PP and EP. The second regime is projected for parts of the Southern Ocean: an alleviation of light and/or temperature limitation leads to an increase in PP and EP as productivity is fueled by a sustained nutrient input. A region of disagreement among the models is the Arctic, where three models project an increase in PP while one model projects a decrease. Projected changes in seasonal and interannual variability are modest in most regions. Regional model skill metrics are proposed to generate multi-model mean fields that show an improved skill in representing observation-based estimates compared to a simple multi-model average. Model results are compared to recent productivity projections with three different algorithms, usually applied to infer net primary production from satellite observations.

Citation: Steinacher, M., Joos, F., Frölicher, T. L., Bopp, L., Cadule, P., Cocco, V., Doney, S. C., Gehlen, M., Lindsay, K., Moore, J. K., Schneider, B., and Segschneider, J.: Projected 21st century decrease in marine productivity: a multi-model analysis, Biogeosciences, 7, 979-1005, doi:10.5194/bg-7-979-2010, 2010.
Publications Copernicus