Journal cover Journal topic
Earth System Dynamics An interactive open-access journal of the European Geosciences Union

Journal metrics

  • IF value: 3.635 IF 3.635
  • IF 5-year<br/> value: 3.869 IF 5-year
  • CiteScore<br/> value: 4.15 CiteScore
  • SNIP value: 0.995 SNIP 0.995
  • SJR value: 2.742 SJR 2.742
  • IPP value: 3.679 IPP 3.679
  • h5-index value: 21 h5-index 21
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
29 Aug 2014
Review status
This discussion paper has been under review for the journal Earth System Dynamics (ESD). The revised manuscript was not accepted.
Differences in carbon cycle and temperature projections from emission- and concentration-driven earth system model simulations
P. Shao1, X. Zeng1, and X. Zeng2 1International Center for Climate and Environment Sciences, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
2Department of Atmospheric Sciences, University of Arizona, Tucson, AZ, USA
Abstract. The influence of prognostic and prescribed atmospheric CO2 concentrations ([CO2]) on the carbon uptake and temperature is investigated using all eight Earth System Models (ESMs) with relevant output variables from the Coupled Model Intercomparison Project Phase 5 (CMIP5). Under the RCP8.5 scenario, the projected [CO2] differences in 2100 vary from −19.7 to +207.3 ppm in emission-driven ESMs. Incorporation of the interactive concentrations also increases the range of global warming, computed as the 20 year average difference between 2081–2100 and 1850–1869/1861–1880, by 49% from 2.36 K (i.e. ranging from 3.11 to 5.47 K) in the concentration-driven simulations to 3.51 K in the emission-driven simulations. The observed seasonal amplitude of global [CO2] from 1980–2011 is about 1.2–5.3 times as large as those from the eight emission-driven ESMs, while the [CO2] seasonality is simply neglected in concentration-driven ESMs, suggesting the urgent need of ESM improvements in this area. The temperature-concentration feedback parameter α is more sensitive to [CO2] (e.g. during 1980–2005 versus 2075–2100) than how [CO2] is handled (i.e. prognostic versus prescribed). This sensitivity can be substantially reduced by using a more appropriate parameter α' computed from the linear regression of temperature change versus that of the logarithm of [CO2]. However, the inter-model relative variations of both α and α' remain large, suggesting the need of more detailed studies to understand and hopefully reduce these discrepancies.

Citation: Shao, P., Zeng, X., and Zeng, X.: Differences in carbon cycle and temperature projections from emission- and concentration-driven earth system model simulations, Earth Syst. Dynam. Discuss., 5, 991-1012,, 2014.
P. Shao et al.
P. Shao et al.


Total article views: 552 (including HTML, PDF, and XML)

HTML PDF XML Total BibTeX EndNote
362 152 38 552 15 33

Views and downloads (calculated since 29 Aug 2014)

Cumulative views and downloads (calculated since 29 Aug 2014)



Latest update: 23 Jun 2017
Publications Copernicus