摘要
The IPCC SRES narratives were implemented in IMAGE 2.2 to evaluate thefuture condition of the climate system (including the biosphere). A series of scenario experiments was used to assess possible ranges in emissions and concentrations of greenhouse gases, climate change and impacts. These experiments focussed on the role of the terrestrial carbon cycle. The experiments show that the SRES narratives dominate human emissions and not natural processes. In contrary, atmospheric CO2 concentration strongly differs between the experiments. Atmospheric CO2 concentrations range for A1B from 714 to 1009 ppmv CO2 in 2100. The spread of this range is comparable with the full SRES range as implemented in IMAGE 2.2 (515-895 μmol/mol CO2). The most important negative and positive feedback processes in IMAGE 2.2 on the build-up of CO2 concentrations are CO2 fertilisation and soil respiration respectively. Indirect effects of these processes furtherchange land-use patterns, deforestation rates and alter the natural C fluxes. The cumulative effects of these changes have a pronounced influence on the final CO2 concentrations. Our scenario experiments highlight the importance of a proper parameterisation of feedback processes, C-cycle and land use in determining the future states of the climate system.
The IPCC SRES narratives were implemented in IMAGE 2.2 to evaluate the future con- dition of the climate system (including the biosphere). A series of scenario experiments was used to assess possible ranges in emissions and concentrations of greenhouse gases, climate change and impacts. These experiments focussed on the role of the terrestrial carbon cycle. The experi- ments show that the SRES narratives dominate human emissions and not natural processes. In contrary, atmospheric CO_2 concentration strongly differs between the experiments. Atmospheric CO_2 concentrations range for A1B from 714 to 1009 ppmv CO_2 in 2100. The spread of this range is comparable with the full SRES range as implemented in IMAGE 2.2 (515-895 μmol/mol CO_2). The most important negative and positive feedback processes in IMAGE 2.2 on the build-up of CO_2 concentrations are CO_2 fertilisation and soil respiration respectively. Indirect effects of these processes further change land-use patterns, deforestation rates and alter the natural C fluxes. The cumulative effects of these changes have a pronounced influence on the final CO_2 concentrations. Our scenario experiments highlight the importance of a proper parameterisation of feedback proc- esses, C-cycle and land use in determining the future states of the climate system.
