Details

Autor(en) / Beteiligte

• Zickfeld, Kirsten
• Eby, Michael
• Weaver, Andrew J.
• Alexander, Kaitlin
• Crespin, Elisabeth
• Edwards, Neil R.
• Eliseev, Alexey V.
• Feulner, Georg
• Fichefet, Thierry
• Forest, Chris E.
• Friedlingstein, Pierre
• Goosse, Hugues
• Holden, Philip B.
• Joos, Fortunat
• Kawamiya, Michio
• Kicklighter, David
• Kienert, Hendrik
• Matsumoto, Katsumi
• Mokhov, Igor I.
• Monier, Erwan
• Olsen, Steffen M.
• Pedersen, Jens O. P.
• Perrette, Mahe
• Philippon-Berthier, Gwenaëlle
• Ridgwell, Andy
• Schlosser, Adam
• Von Deimling, Thomas Schneider
• Shaffer, Gary
• Sokolov, Andrei
• Spahni, Renato
• Steinacher, Marco
• Tachiiri, Kaoru
• Tokos, Kathy S.
• Yoshimori, Masakazu
• Zeng, Ning
• Zhao, Fang

Titel

Long-Term Climate Change Commitment and Reversibility: An EMIC Intercomparison

Ist Teil von

• Journal of climate, 2013-08, Vol.26 (16), p.5782-5809

Ort / Verlag

Boston: American Meteorological Society

Erscheinungsjahr

2013

Quelle

EZB Free E-Journals

Beschreibungen/Notizen

• This paper summarizes the results of an intercomparison project with Earth System Models of Intermediate Complexity (EMICs) undertaken in support of the Intergovernmental Panel on Climate Change (IPCC) Fifth Assessment Report (AR5). The focus is on long-term climate projections designed to 1) quantify the climate change commitment of different radiative forcing trajectories and 2) explore the extent to which climate change is reversible on human time scales. All commitment simulations follow the four representative concentration pathways (RCPs) and their extensions to year 2300. Most EMICs simulate substantial surface air temperature and thermosteric sea level rise commitment following stabilization of the atmospheric composition at year-2300 levels. The meridional overturning circulation (MOC) is weakened temporarily and recovers to near-preindustrial values in most models for RCPs 2.6–6.0. The MOC weakening is more persistent for RCP8.5. Elimination of anthropogenic CO₂ emissions after 2300 results in slowly decreasing atmospheric CO₂ concentrations. At year 3000 atmospheric CO₂ is still at more than half its year-2300 level in all EMICs forRCPs 4.5–8.5. Surface air temperature remains constant or decreases slightly and thermosteric sea level rise continues for centuries after elimination of CO₂ emissions in all EMICs. Restoration of atmospheric CO₂ from RCP to preindustrial levels over 100–1000 years requires large artificial removal of CO₂ from the atmosphere and does not result in the simultaneous return to preindustrial climate conditions, as surface air temperature and sea level response exhibit a substantial time lag relative to atmospheric CO₂.