Quantifying non-CO2 contributions to remaining carbon budgets

被引:10
|
作者
Jenkins, Stuart [1 ]
Cain, Michelle [1 ,2 ]
Friedlingstein, Pierre [3 ,4 ]
Gillett, Nathan [5 ]
Walsh, Tristram [1 ]
Allen, Myles R. [1 ,6 ]
机构
[1] Univ Oxford, Dept Phys, AOPP, Oxford, England
[2] Cranfield Univ, Ctr Environm & Agr Informat, Cranfield, Beds, England
[3] Univ Exeter, Coll Engn Math & Phys Sci, Exeter EX4 4QF, Devon, England
[4] Ecole Normale Super, CNRS, Lab Meteorol Dynam, UPMC X,ENS,Inst Pierre Simon Laplace, 24 Rue Lhomond, F-75005 Paris, France
[5] Environm & Climate Change Canada, Canadian Ctr Climate Modelling & Anal, Victoria, BC, Canada
[6] Univ Oxford, Sch Geog, Environm Change Inst, Oxford, England
关键词
ZERO EMISSIONS; CLIMATE; TEMPERATURE; COMMITMENT; PROTOCOL; DIOXIDE; METRICS; CO2;
D O I
10.1038/s41612-021-00203-9
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The IPCC Special Report on 1.5 degrees C concluded that anthropogenic global warming is determined by cumulative anthropogenic CO2 emissions and the non-CO2 radiative forcing level in the decades prior to peak warming. We quantify this using CO2-forcing-equivalent (CO2-fe) emissions. We produce an observationally constrained estimate of the Transient Climate Response to cumulative carbon Emissions (TCRE), giving a 90% confidence interval of 0.26-0.78 degrees C/TtCO(2), implying a remaining total CO2-fe budget from 2020 to 1.5 degrees C of 350-1040 GtCO(2)-fe, where non-CO2 forcing changes take up 50 to 300 GtCO(2)-fe. Using a central non-CO2 forcing estimate, the remaining CO2 budgets are 640, 545, 455 GtCO(2) for a 33, 50 or 66% chance of limiting warming to 1.5 degrees C. We discuss the impact of GMST revisions and the contribution of non-CO2 mitigation to remaining budgets, determining that reporting budgets in CO2-fe for alternative definitions of GMST, displaying CO2 and non-CO2 contributions using a two-dimensional presentation, offers the most transparent approach.
引用
收藏
页数:10
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