代表性濃度路徑
參考文獻

↑  . IPCC.   [2019-02-13]. （原始内容存档于2019-02-14）.
↑  Richard Moss;  et al.  (PDF). Geneva: Intergovernmental Panel on Climate Change. 2008: 132  [2023-11-24]. （原始内容存档 (PDF)于2023-11-26）.
↑  Weyant, John; Azar, Christian; Kainuma, Mikiko; Kejun, Jiang; Nakicenovic, Nebojsa; Shukla, P.R.; La Rovere, Emilio; Yohe, Gary.  (PDF). Geneva, Switzerland: IPCC Secretariat. April 2009  [2023-11-24]. （原始内容存档 (PDF)于2023-10-12）.
1 2 3 4 5 6 7 8  . Carbon Brief. 2018-04-19  [2020-03-04]. （原始内容存档于2020-01-07） （英语）.
1 2 3  https://ar5-syr.ipcc.ch/topic_futurechanges.php （页面存档备份，存于） Box 2.2, figure 1
1 2  .   [2023-11-24]. （原始内容存档于2023-10-29）.
1 2 3  Meinshausen, Malte; Smith, S. J.; Calvin, K.; Daniel, J. S.; Kainuma, M. L. T.; Lamarque, J-F.; Matsumoto, K.; Montzka, S. A.; Raper, S. C. B.; Riahi, K.; Thomson, A.; Velders, G. J. M.; van Vuuren, D.P. P. . Climatic Change. 2011, 109 (1–2): 213–241. ISSN 0165-0009. doi:10.1007/s10584-011-0156-z （英语）.
1 2  . Carbon Brief. 2018-04-19  [2023-11-24]. （原始内容存档于2020-01-07）.
1 2 3 4  Collins, M., et al.: Section 12.3.1.3 The New Concentration Driven RCP Scenarios, and their Extensions, in: Chapter 12: Long-term Climate Change: Projections, Commitments and Irreversibility （页面存档备份，存于）(archived ), in IPCC AR5 WG1 （页面存档备份，存于）, p. 1045–1047
↑   (PDF) (报告). the uncertainty is now estimated to be smaller than with the AR4 method for long-term climate change, because the carbon cycle–climate feedbacks are not relevant for the concentration-driven RCP projections []
↑   (PDF) (报告). With very high confidence, ocean carbon uptake of anthropogenic CO2 emissions will continue under all four Representative Concentration Pathways (RCPs) through to 2100, with higher uptake corresponding to higher concentration pathways. The future evolution of the land carbon uptake is much more uncertain, with a majority of models projecting a continued net carbon uptake under all RCPs, but with some models simulating a net loss of carbon by the land due to the combined effect of climate change and land use change. In view of the large spread of model results and incomplete process representation, there is low confidence on the magnitude of modelled future land carbon changes. []
↑  Ward, James D.; Mohr, Steve H.; Myers, Baden R.; Nel, William P. . Energy Policy. December 2012, 51: 598–604. doi:10.1016/j.enpol.2012.09.003.
1 2  https://ar5-syr.ipcc.ch/topic_futurechanges.php （页面存档备份，存于） Box 2.2
1 2  Pielke JR., Roger. . osf.io. 2021-04-10  [2021-04-26]. S2CID 241829692. doi:10.31235/osf.io/m4fdu . （原始内容存档于2023-10-29）.
↑  Höök M, Sivertsson A, Aleklett K. . Natural Resources Research. 2010-02-18, 19 (2): 63–81  [2021-10-10]. S2CID 14389093. doi:10.1007/s11053-010-9113-1. It is found that the SRES unnecessarily takes an overoptimistic stance and that future production expectations are leaning toward spectacular increases from present output levels. In summary, we can only encourage the IPCC to involve more resource experts and natural science in future emission scenarios.
↑  Laherrère, Jean.  (PDF). EMF/IEA/IEW meeting. IIASA. 2001-06-10  [2021-10-10]. （原始内容存档 (PDF)于2023-10-29）. It is obvious that the IPCC assumptions for oil and gas are based on the assumption of abundant cheap oil and gas. This concept has to be revised.
↑  https://ar5-syr.ipcc.ch/topic_summary.php （页面存档备份，存于） table SPM.1
↑  https://ar5-syr.ipcc.ch/topic_futurechanges.php （页面存档备份，存于） 2.3.1
↑  . Science On a Sphere.   [2022-05-30]. （原始内容存档于2023-10-10） （英语）.
↑  Hausfather, Zeke; Peters, Glen. . Nature. 2020-01-29, 577 (7792): 618–20. Bibcode:2020Natur.577..618H. PMID 31996825. doi:10.1038/d41586-020-00177-3 .
↑  . BBC.   [2020-03-05]. （原始内容存档于2023-10-29） （英国英语）.
↑  Schwalm, Christopher R.; Glendon, Spencer; Duffy, Philip B. . Proceedings of the National Academy of Sciences. 2020-08-18, 117 (33): 19656–19657. Bibcode:2020PNAS..11719656S. ISSN 0027-8424. PMC 7443890 . PMID 32747549. doi:10.1073/pnas.2007117117  （英语）.
1 2 3  IPCC: Table SPM-2, in: Summary for Policymakers （页面存档备份，存于）(archived ), in IPCC AR5 WG1 （页面存档备份，存于）
1 2  Collins, Matthew, et al.: Executive summary, in: Chapter 12: Long-term Climate Change: Projections, Commitments and Irreversibility （页面存档备份，存于） (archived 2014-07-16), in IPCC AR5 WG1 （页面存档备份，存于）, p. 1033