Articles | Volume 12, issue 10
Model experiment description paper
15 Oct 2019
Model experiment description paper |  | 15 Oct 2019

The Zero Emissions Commitment Model Intercomparison Project (ZECMIP) contribution to C4MIP: quantifying committed climate changes following zero carbon emissions

Chris D. Jones, Thomas L. Frölicher, Charles Koven, Andrew H. MacDougall, H. Damon Matthews, Kirsten Zickfeld, Joeri Rogelj, Katarzyna B. Tokarska, Nathan P. Gillett, Tatiana Ilyina, Malte Meinshausen, Nadine Mengis, Roland Séférian, Michael Eby, and Friedrich A. Burger

The amount of additional future temperature change following a complete cessation of CO2 emissions is a measure of the unrealized warming to which we are committed due to CO2 already emitted to the atmosphere. This “zero emissions commitment” (ZEC) is also an important quantity when estimating the remaining carbon budget – a limit on the total amount of CO2 emissions consistent with limiting global mean temperature at a particular level. In the recent IPCC Special Report on Global Warming of 1.5 C, the carbon budget framework used to calculate the remaining carbon budget for 1.5 C included the assumption that the ZEC due to CO2 emissions is negligible and close to zero. Previous research has shown significant uncertainty even in the sign of the ZEC. To close this knowledge gap, we propose the Zero Emissions Commitment Model Intercomparison Project (ZECMIP), which will quantify the amount of unrealized temperature change that occurs after CO2 emissions cease and investigate the geophysical drivers behind this climate response. Quantitative information on ZEC is a key gap in our knowledge, and one that will not be addressed by currently planned CMIP6 simulations, yet it is crucial for verifying whether carbon budgets need to be adjusted to account for any unrealized temperature change resulting from past CO2 emissions. We request only one top-priority simulation from comprehensive general circulation Earth system models (ESMs) and Earth system models of intermediate complexity (EMICs) – a branch from the 1 % CO2 run with CO2 emissions set to zero at the point of 1000 PgC of total CO2 emissions in the simulation – with the possibility for additional simulations, if resources allow. ZECMIP is part of CMIP6, under joint sponsorship by C4MIP and CDRMIP, with associated experiment names to enable data submissions to the Earth System Grid Federation. All data will be published and made freely available.

Please read the corrigendum first before continuing.

1 Introduction

The zero emissions commitment (ZEC), or the amount of global mean temperature change that is still expected to occur after a complete cessation of CO2 emissions, is a key component of estimating the remaining carbon budget to stay within global warming targets as well as an important metric to understand impacts and reversibility of climate change (Matthews and Solomon, 2013). Much effort is put into measuring and constraining the TCRE – the Transient Climate Response to cumulative CO2 Emissions (Allen et al., 2009; Matthews et al., 2009; Zickfeld et al., 2009; Raupach et al., 2011; Gillett et al., 2013; Tachiiri et al., 2015; Goodwin et al., 2015; Steinacher and Joos, 2016; MacDougall, 2016; Ehlert et al., 2017; Millar and Friedlingstein, 2018). The TCRE describes the ratio between CO2-induced warming and cumulative CO2 emissions up to the same point in time, but it does not capture any delayed warming response to CO2 emissions beyond the point that emissions reach zero. When using the TCRE to derive the carbon budget consistent with a specific temperature limit, the ZEC is often assumed to be negligible and close to zero (Matthews et al., 2017; Rogelj et al., 2011, 2018). Constraints on ZEC have not been systematically researched so far, although both TCRE and ZEC are required to relate carbon emissions to the eventual equilibrium warming (Rogelj et al., 2018).

It has been shown that continued CO2 removal by natural sinks following cessation of emissions offsets the continued warming that would result from stabilized CO2 concentration (Matthews and Caldeira, 2008; Solomon et al., 2009; Frölicher and Joos, 2010; Matthews and Weaver, 2010; Joos et al., 2013). This is partly due to the ocean uptake of both heat and carbon sharing some similar processes and timescales, and it is therefore expected to lead to ZEC being small (Allen et al., 2018; Ehlert and Zickfeld, 2017; Gillett et al., 2011; Matthews and Zickfeld, 2012). This has been shown to be a general result across a range of models (Gillett et al., 2011; Lowe et al., 2009; Matthews and Zickfeld, 2012; Zickfeld et al., 2013). Most such literature focused on long timescales (up to and beyond a century). This led IPCC SR15 (Rogelj et al., 2018) to make the assumption for the estimation of carbon budgets that for timescales up to a century ZEC was uncertain, yet centred around zero. More detailed studies, however, have shown that ZEC can be (a) non-zero, possibly of either positive or negative sign that may change in time during the period following emissions ceasing (Frölicher et al., 2014; Frölicher and Paynter, 2015), and (b) it is both state and rate dependent – i.e. it varies depending on the amount of carbon emitted and taken up by the natural carbon sinks, and the CO2 emissions pathway of its emissions prior to cessation (Ehlert and Zickfeld, 2017; Krasting et al., 2014; MacDougall, 2019).

When we consider stringent climate targets, such as limiting global mean warming to 1.5 or 2 C, and in light of approximately 1 C warming to date and potential future warming from non-CO2 greenhouse gases, an uncertainty in ZEC of 0±0.1C already leads to a substantial uncertainty in the remaining carbon budget. Given the current central estimate of the TCRE of 1.6 C per 1000 PgC (Collins et al., 2013), each 0.1 C of warming equates to approximately 60 PgC of CO2 emissions, or approximately 6 years of current fossil fuel emission rates (Le Quéré et al., 2018). It has therefore emerged that quantitative information on ZEC is a key gap in our knowledge, and one that is not filled by currently planned simulations for the sixth phase of the Coupled Model Intercomparison Project (CMIP6).

ZECMIP aims to fill this gap as efficiently as possible. Thereby, ZECMIP will support the assessment of remaining carbon budgets based on the CMIP6 simulations and supersede the current practice of applying a single model estimate of ZEC or an estimate from a limited number of studies from the literature. Much more preferable is to coordinate parallel studies, with Earth system general circulation models (ESMs) and Earth system models of intermediate complexity (EMICs), to measure both TCRE and ZEC in a common scenario. Hence, we proposed using the 1 % per annum increase in CO2 concentration experiment (1pctCO2) from the CMIP6 Diagnostic Evaluation and Characterization of Klima (DECK) simulations (Eyring et al., 2016) as a common baseline simulation for estimating both the TCRE and the ZEC.

Table 1ZECMIP simulations and priorities for ESMs and EMICs.

Download Print Version | Download XLSX

As a late addition to CMIP6, ZECMIP has been designed to address this important question with only one high-priority simulation – A1: “a zero-emission experiment following 1000 PgC emissions” – implemented as a branching off from the 1pctCO2 simulation from the point at which 1000 PgC in diagnosed cumulative emissions is reached. Additional simulations of lower priority are also suggested, which will aid further analysis. Branching from this idealized simulation avoids complications of non-CO2 forcing and land-use or nitrogen deposition impacts on the carbon cycle, and also makes the quantified ZEC consistent with the TCRE values also derived from this simulation.

This paper documents the ZECMIP simulations with a focus on the details needed for ESMs and EMICs to contribute the top-priority simulation of a ZEC run from the point of 1000 PgC emissions following 1 % per year growth in CO2.

ZECMIP analysis will draw on carbon cycle feedbacks and process understanding from C4MIP (Coupled Climate Carbon Cycle Model Intercomparison Project; Jones et al., 2016) and aims to complement analysis on reversibility and CO2 removal under CDRMIP (Carbon Dioxide Removal Model Intercomparison Project; Keller et al., 2018). Both C4MIP and CDRMIP encourage participation in the ZECMIP top-priority simulation. For simplicity, the data request is a replica of that for the CMIP6 emission-driven historical simulation (esm-hist). No new variables have been added. For EMICs the request is to output the same model variables as from the 1 % run, which forms the basis of ZECMIP, with the one addition of also providing atmospheric CO2 concentration. Data can be published via the Earth System Grid Federation (ESGF) (for ESMs contributing to CMIP6). An equivalent data repository will be available for EMICs and likely based at the University of Victoria – details will be communicated during summer 2019 via C4MIP and CDRMIP websites.

2 Simulation protocol

Due to time pressures and a limit to computational resources for modelling groups, ZECMIP has just one high-priority simulation, with a second lower-priority simulation suggested (See Table 1). Other lower-priority simulations are also detailed and welcomed. For EMIC model groups, there is an extended protocol with longer and additional experiments. We welcome ESM groups to also perform these additional simulations, but this is not required. Given that the overall CMIP6 protocol (Eyring et al., 2016) has been years in development, it is not possible to initiate a new MIP nor allocate new CMIP tier-1 simulations during 2019. Instead, ZECMIP simulations are being included under C4MIP and CDRMIP and included in CMIP as tier-2 and tier-3 simulations so that they do not become mandatory “entry card” requirements for C4MIP or CDRMIP. Hence, our top-priority simulation, A1, is classed as a CMIP tier-2 simulation; all others are classified as tier-3 simulations. However, Table 1 lists the simulations prioritized by ZECMIP to guide groups who have limited resources to perform the simulations. We hope as many groups as possible perform as many of the simulations as possible, and participating model groups will be offered co-authorship on the article containing the analysis to be submitted this year (by December 2019).

2.1 Simulation set A: abrupt zero emissions

All ZECMIP simulations are required to be in “emissions-driven mode”. Experiments under set A require branching off from a simulation where CO2 concentration follows a 1 % per annum increase from pre-industrial levels. This presents model groups with a choice of how to initialize experiments A1 to A3. Some models may have the capability to switch from concentration-driven to emissions-driven configurations but some models may not or model groups may not have confidence that they can do so without a shock to the model system. In the case of the former, the concentration-driven DECK 1pctCO2 simulation can be used to initiate experiments A1 to A3. Otherwise, models should perform simulation A0 to generate initial conditions for A1 to A3.

We do not specify a precise definition of how to make this choice but suggest that when an emissions-driven control run is initiated from a concentration-driven control run, any subsequent change in atmospheric CO2, major carbon stores, or global temperature should all be approximately within the expected interannual variability of the control run. We note that if simulation A0 is required to initialize the A1 simulation, then it should be treated as equal priority to A1 and data submission to the ESGF is required.

A0: “esm-1pctCO2”. Run an emissions-driven version of 1pctCO2 to get to the branch-off point for A1 to A3. The requirement to run this is a model-by-model decision. The compatible emissions time series for this simulation should be calculated from the 1pctCO2 and used to branch esm-1pctCO2 from esm-piControl to replicate the 1 % profile as closely as possible up to the desired cumulative emission before setting emissions to zero from this point.

The compatible emission rate E (PgC yr−1) can be calculated from the 1pctCO2 concentration-driven simulation, as described in Jones et al. (2013; see their Sect. 2b). In summary, changes in atmospheric CO2 concentration (CA) are balanced by anthropogenic emissions, E, and changes in the natural land and ocean carbon reservoirs (CL and CO, respectively). Therefore, the compatible emissions can be calculated simply as


where units of all quantities are in petagrams of carbon (PgC). Changes in atmospheric CO2 can be converted from concentration (ppm) to mass (PgC) by a simple scaling of 2.12. Typically, the time derivative, d∕dt, is taken to imply changes per year – i.e. annual changes in the carbon stores are used in order to calculate annual emission, E. The calculation is done using global total amounts. Emissions should be prescribed as globally uniform at the surface. Models that have run multiple ensemble members for the concentration-driven 1pctCO2 experiment should use ensemble-mean values of CL and CO from those runs to derive the emissions for forcing the esm-1pctCO2 simulation. This will minimize the effect of interannual variability of carbon sinks on the diagnosed compatible emissions. If desired, numerical smoothing of the global mean time series of emissions may also be applied as long as the cumulative total is not affected.

Figure 1Example results from simulation A1 from the UVic ESCM (Weaver et al., 2001; MacDougall and Knutti, 2016; blue) and GFDL-ESM2M (Dunne et al., 2012, 2013; red) models. (a) CO2 concentration prescribed (black line) in the 1pctCO2 simulation and simulated (red, blue lines) by the two models; (b) simulated global mean surface air temperature for the same period; (c) global mean temperature response from the branch point off the 1 % simulation with zero subsequent emissions.


ZECMIP simulation set A is based on CO2-only 1 % run (either concentration-driven DECK “1pctCO2” or the above described A.0 “esm-1pctCO2”), with all the other external forcing held at pre-industrial conditions (i.e. non-CO2 greenhouse gases, aerosols, volcanoes, land-use changes, solar irradiance). After following the CO2 concentration up to the level described below, branch off with prognostic CO2 (a.k.a. “emissions driven”) but with carbon emissions set to zero (E=0). Simulate the subsequent reduction in atmospheric CO2 and change in climate for at least 100 years.

Branch off at the following given cumulative emissions.

  • A1: “esm-1pct-brch-1000PgC”, 1000 PgC. This is the ZECMIP top-priority simulation. This corresponds to approximately 2 C CO2-induced warming above pre-industrial levels (with the year 1850 here taken as proxy for pre-industrial levels). Figure 1 shows example results from two models.

  • A2: “esm-1pct-brch-750PgC”, 750 PgC. This is a simulation corresponding to approximately 1.5 C CO2-induced warming above 1850 and is optional.

  • A3: “esm-1pct-brch-2000PgC”, 2000 PgC. This simulation will give insights into ZEC for a possible higher CO2-induced warming and is optional.

The experimental design is for all models to branch off at a common cumulative carbon emission level, acknowledging that this will mean a different year for ceasing emissions and thus a slightly different atmospheric CO2 concentration and departure of global mean temperature from 1850 for each model at the beginning of the ZECMIP simulations. EMICs should run the simulations for at least 1000 years. We anticipate that the small signal-to-noise ratio of the ZEC versus the internal climate variability may require an ensemble of simulations. However, acknowledging ESM time pressure and limits to computational resources, only one ensemble member is required.

Figure 2Time series of global CO2 emissions for bell-shaped curve pathways B1 to B3. The numbers in the legend indicate the cumulative amount of CO2 emissions for each simulation.


Experiment A1 aims to quantify ZEC at 1000 PgC (cumulative emissions) at which point TCRE will be calculated. A2 and A3 explore the state dependence of ZEC at approximately 1.5 C CO2-induced warming above 1850 and at significantly higher cumulative emissions, respectively.

Figure 3Example results from simulation B1 from the UVic ESCM (Weaver et al., 2001; MacDougall and Knutti, 2016; blue) and GFDL-ESM2M (Dunne et al., 2012, 2013; red) models. (a) CO2 concentration simulated by the two models; (b) simulated global mean surface air temperature for the same period; (c) global mean temperature response from year 100 onwards with zero subsequent emissions.


2.2 Simulation set B: bell-shaped zero emissions

This second set of experiments, B1 to B3, aims to explore the dependence of ZEC on CO2 emissions rate by following a pathway emitting the same cumulative emissions as A1 to A3 but with a smooth transition to zero emissions, followed by 100 years of E=0 (EMICs for at least 1000 years). The main purpose of this experiment is to quantify the dependency of ZEC on emission pathways and the emission rate prior to the point when TCRE is evaluated as the Earth system is subject to comparatively low emissions, occurring just before the TCRE evaluation point of zero emissions after 100 years of simulation – compared to the sudden cessation of high emissions in experiments A1, A2, and A3.

The conventional way of estimating TCRE is using 1 % CO2 model simulations. The tier-1 A1 simulation thus provides the most complementary and internally consistent quantification of the ZEC, which is why we consider this to be the top priority. However, additional ZECMIP experiments with more gradually phased out emissions enable us to determine how the ZEC is expected to materialize over the timescales of more societally relevant CO2 emissions reduction rates. Analysis of pairs of A and B experiments will allow us to generalize the findings for other emission reduction pathways, allowing us to answer the question of whether temperature will continue to increase following a more realistic cessation of CO2 emissions.

These B experiments are run in emissions-driven configuration (CO2-only: following 1pctCO2 and piControl, all other external forcing is fixed at pre-industrial levels), assuming a bell-shaped emissions profile (Fig. 2), for which we have chosen an arbitrary Gaussian distribution (see Appendix A). At the end of 100 years emissions profile, simulations should continue with zero emissions for at least 100 years (for ESMs) or 1000 years (EMICs).

The bell-shaped curve is designed to give the following cumulative emissions.

  • B1: “esm-bell-1000PgC”, 1000 PgC (Fig. 3 shows example results from two models);

  • B2: “esm-bell-750PgC”, 750 PgC;

  • B3: “esm-bell-2000PgC”, 2000 PgC.

By design, this set B utilizes the same cumulative emissions as the respective simulations in set A experience up to their branch point. These emissions are applied over 100 years, followed by zero emissions for 100 years (ESMs) or 1000 years (EMICs). These additional simulations allow for a direct comparison of the two ZEC experiment sets, given the same amount of cumulative emissions. A model decision is required on the spatial pattern of emissions – we suggest globally uniform at surface. The time series of global CO2 emissions for the above curves is listed in Appendix A and is hosted on the C4MIP (, last access: 6 September 2019) and CDRMIP (, last access: 6 September 2019) websites.

3 ZECMIP outlook and conclusions

The experiments outlined above will lay the foundation for coordinated multi-model analysis of the zero emissions commitment. The absence of a dedicated experiment to quantify ZEC across CMIP models was identified and is addressed by our top-priority experiment, A1. Investigations into the state, rate, and pathway dependence of the ZEC are aided by further experiments with sudden and gradual cessation of emissions. ZECMIP was motivated to keep the experiment design both lightweight and simple to follow; in future, further simulations could be defined to explore additional issues such as cessation of emissions of non-CO2 greenhouse gases, aerosols, or from land-use activities. The complexity of defining such experiments precluded an exhaustive inclusion in this first generation of ZECMIP but we acknowledge the importance of rate and pathway dependency, as well non-CO2 aspects in determining ZEC and the remaining carbon budget overall (MacDougall et al., 2015; Rogelj et al., 2015; Mengis et al., 2018; Tokarska et al., 2018).

The requirement for specific information regarding ZEC to assess remaining carbon budgets was identified in the IPCC Special Report on Global Warming of 1.5 C (Rogelj et al., 2018). An initial paper exploring ZEC in this context, explicitly on timescales of relevance to 21st century carbon budgets, is planned on a timeline that could support an improved assessment of the ZEC and its influence on carbon budgets in the IPCC Sixth Assessment Report. All participating model groups who are able to complete and provide data for simulation A1 in time will be invited to join this analysis.

ZECMIP welcomes community engagement in the participation of simulations and their analysis, as well as input to future analysis and experimental design. We hope to bring together ESMs and EMICs to enable analysis across timescales from decadal through centennial to millennial.

Furthermore, as a set of numerical simulations, ZECMIP is intended to complement existing CMIP activity, especially on carbon cycle feedbacks, CO2 removal, and reversibility of the climate system. C4MIP simulations aim to address model evaluation during the historical period from 1850 to present day, along with process-level feedback analysis. CDRMIP adds to this with exploration of the processes controlling the response of the climate and carbon cycle to negative emissions and reversibility of components of the Earth system. ZECMIP will contribute additional simulations and analysis to aid understanding of the mechanisms of the climate response to CO2 emissions and relationships between transient and equilibrium climate sensitivities. We hope that ZECMIP analysis will address the crucial knowledge gap surrounding committed warming following ceasing emissions and will provide valuable support for assessment of carbon budgets to achieve climate targets.

Data availability

As with all CMIP6-endorsed MIPs, the model output from the ZECMIP simulations described in this paper will be distributed through the Earth System Grid Federation (ESGF) with version control and digital object identifiers (DOIs) assigned. No additional model forcings are required beyond those already used for piControl and 1pctCO2 simulations apart from the emission inputs for the proposed B experiments, which are described in Appendix A of this paper and are hosted on the C4MIP and CDRMIP websites.

Appendix A:CO2 emissions for bell-shaped curve simulations B1–3

This table lists the global CO2 emissions (PgC yr−1) to be applied for the first 100 years of simulations B1–3. This period should be followed by at least 100 years of zero emissions for ESMs or 1000 years for EMICs (see Fig. 2). These emissions should be prescribed as globally uniform at the surface.

The data were calculated from a Gaussian curve according to


where emissions, E, are scaled by a constant, k, so that the cumulative total matches the required amount for each scenario (1000 PgC for B1, 750 PgC for B2, 2000 PgC for B3). The parameters were set as μ=50 as the centre of the 100-year period and σ=100/6 so that the distribution spans 3 standard deviations about the centre.

These data in .csv file format are available from the C4MIP (, last access: 6 September 2019) and CDRMIP (, last access: 6 September 2019) websites.

Table A1Global CO2 emissions (PgC yr−1) to be applied during each year for the first 100 years of simulations B1–3.

Download XLSX

Author contributions

CDJ, TLF, CK, AHM, HDM, KZ, JR, KBT, NPG, TI, MM, NM, and RS participated in workshop discussions to identify research needs towards better understanding of remaining carbon budgets. ZECMIP was the direct outcome of this workshop and the participants were all active in breakout discussions to design the experimental protocol described here. ME was instrumental in providing support and data storage for EMIC simulations and provided valuable guidance around the data request detailed in the article. FAB performed simulations with GFDL-ESM2M to specifically test the experimental design and provide data for Figs. 1 and 3. All authors contributed to the development of the article, provided text, and responded to review comments and revisions.

Competing interests

The authors declare that they have no conflict of interest.


This protocol was devised at a Global Carbon Project workshop supported by H2020 EU project CRESCENDO under grant agreement no. 641816. Chris D. Jones was supported by the Joint UK BEIS/Defra Met Office Hadley Centre Climate Programme (GA01101). Joeri Rogelj, Katarzyna Tokarska and Roland Séférian were supported by H2020 EU project CONSTRAIN under grant agreement no. 820829. Tatiana Ilyina and Thomas L. Frölicher were supported by H2020 EU project CCICC under grant agreement no. 821003. Thomas L. Frölicher acknowledges support from the Swiss National Science Foundation under grant PP00P2_170687. GFDL-ESM2M simulations were performed at the Swiss National Supercomputing Centre (CSCS). Kirsten Zickfeld and Andrew H. MacDougall acknowledge support from the National Sciences and Engineering Research Council of Canada's Discovery Grants Program. Charles Koven acknowledges support from the US DOE BER Regional & Global Model Analysis programme through the Early Career Research Program and the RUBISCO SFA projects. Katarzyna B. Tokarska was also supported by the UK NERC-funded SMURPHs project (NE/N006143/1).

Financial support

This research has been supported by the European Commission (grant no. CRESCENDO (641816)).

Review statement

This paper was edited by Carlos Sierra and reviewed by two anonymous referees.


Allen, M. R., Frame, D. J., Huntingford, C., Jones, C. D., Lowe, J. A., Meinshausen, M., and Meinshausen, N.: Warming caused by cumulative carbon emissions towards the trillionth tonne, Nature, 458, 1163–1166,, 2009. 

Allen, M. R., Dube, O. P., Solecki, W., Aragón-Durand, F., Cramer, W., Humphreys, S., Kainuma, M., Kala, J., Mahowald, N., Mulugetta, Y., Perez, R., Wairiu, M., and Zickfeld, K.: Chapter 1 Framing and Context, in: Global warming of 1.5 C, An IPCC Special Report on the impacts of global warming of 1.5 C above pre-industrial levels and related global greenhouse gas emission pathways, in the context of strengthening the global response to the threat of climate change, World Meteorological Organization, Geneva, Switzerland, 2018. 

Collins, M., Knutti, R., Arblaster, J., Dufresne, J.-L., Fichefet, T., Friedlingstein, P., Gao, X., Gutowski, W. J., Johns, T., Krinner, G., Shongwe, M., Tebaldi, C., Weaver, A. J., and Wehner, M.: Long-term Climate Change: Projections, Commitments and Irreversibility, in: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, edited by: Stocker, T. F., Qin, D., Plattner, G.-K., Tignor, M., Allen, S. K., Boschung, J., Nauels, A., Xia, Y., Bex, V., and Midgley, P. M., Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, 2013. 

Dunne, J. P., John, J. G., Adcroft, A. J., Griffies, S. M., Hallberg, R. W., Shevliakova, E. N., Stouffer, R. J., Cooke, W., Dunne, K. A., Harrison, M. J., Krasting, J. P., Levy, H., Malyshev, S. L., Milly, P. C. D., Phillipps, P. J., Sentman, L. T., Samuels, B. L., Spelman, M. J., Winton, M., Wittenberg, A. T., and Zadeh, N.: GFDL's ESM2 global coupled climate-carbon Earth System Models Part I: Physical formulation and baseline simulation characteristics, J. Climate, 25, 6646–6665,, 2012. 

Dunne, J. P., John, J. G., Shevliakova, E., Stouffer, R. J., Krasting, J. P., Malyshev, S. L., Milly, P. C. D., Sentman, L. T., Adcroft, A. J., Cooke, W., Dunne, K. A., Griffies, S. M., Hallberg, R. W., Harrison, M. J., Levy, H., Wittenberg, A. T., Phillips, P. J., and Zadeh, N.: GFDL's ESM2 Global Coupled Climate–Carbon Earth System Models. Part II: Carbon System Formulation and Baseline Simulation Characteristics, J. Climae, 26, 2247–2267,, 2013. 

Ehlert, D. and Zickfeld, K.: What determines the warming commitment after cessation of CO2 emissions?, Environ. Res. Lett., 12, 015002,, 2017. 

Ehlert, D., Zickfeld, K., Eby, M., and Gillett, N.: The sensitivity of the proportionality between temperature change and cumulative CO2 emissions to ocean mixing, J. Climate, 30, 2921–2935,, 2017. 

Eyring, V., Bony, S., Meehl, G. A., Senior, C. A., Stevens, B., Stouffer, R. J., and Taylor, K. E.: Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization, Geosci. Model Dev., 9, 1937–1958,, 2016 

Frölicher, T. L. and Joos, F.: Reversible and irreversible impacts of greenhouse gas emissions in multi-century projections with the NCAR global coupled carbon cycle-climate model, Clim. Dynam., 35, 1439–1459,, 2010. 

Frölicher, T. L. and Paynter, D. J.: Extending the relationship between global warming and cumulative carbon emissions to multi-millennial timescales, Environ. Res. Lett., 10, 075002,, 2015. 

Frölicher, T. L., Winton, M., and Sarmiento, J. L.: Continued global warming after CO2 emissions stoppage, Nat. Clim. Change, 4, 40–44,, 2014. 

Gillett, N. P., Arora, V. K., Zickfeld, K., Marshall, S. J., and Merryfield, W. J.: Ongoing climate change following a complete cessation of carbon dioxide emissions, Nat. Geosci., 4, 83–87,, 2011. 

Gillett, N. P., Arora, V. K., Matthews, D., and Allen, M. R.: Constraining the ratio of global warming to cumulative CO2 emissions using CMIP5 simulations, J. Climate, 26, 6844–6858,, 2013. 

Goodwin, P., Williams, R. G., and Ridgwell, A.: Sensitivity of climate to cumulative carbon emissions due to compensation of ocean heat and carbon uptake, Nat. Geosci., 8, 29–34,, 2015. 

Jones, C., Robertson, E., Arora, V., Friedlingstein, P., Shevliakova, E., Bopp, L., Brovkin, V., Hajima, T., Kato, E., Kawamiya, M., Liddicoat, S., Lindsay, K., Reick, C. H., Roelandt, C., Segschneider, J., and Tjiputra, J.: Twenty-First-Century Compatible CO2 Emissions and Airborne Fraction Simulated by CMIP5 Earth System Models under Four Representative Concentration Pathways, J. Climate, 26, 4398–4413,, 2013. 

Jones, C. D., Arora, V., Friedlingstein, P., Bopp, L., Brovkin, V., Dunne, J., Graven, H., Hoffman, F., Ilyina, T., John, J. G., Jung, M., Kawamiya, M., Koven, C., Pongratz, J., Raddatz, T., Randerson, J. T., and Zaehle, S.: C4MIP – The Coupled Climate-Carbon Cycle Model Intercomparison Project: experimental protocol for CMIP6, Geosci. Model Dev., 9, 2853–2880,, 2016. 

Joos, F., Roth, R., Fuglestvedt, J. S., Peters, G. P., Enting, I. G., von Bloh, W., Brovkin, V., Burke, E. J., Eby, M., Edwards, N. R., Friedrich, T., Frölicher, T. L., Halloran, P. R., Holden, P. B., Jones, C., Kleinen, T., Mackenzie, F. T., Matsumoto, K., Meinshausen, M., Plattner, G.-K., Reisinger, A., Segschneider, J., Shaffer, G., Steinacher, M., Strassmann, K., Tanaka, K., Timmermann, A., and Weaver, A. J.: Carbon dioxide and climate impulse response functions for the computation of greenhouse gas metrics: a multi-model analysis, Atmos. Chem. Phys., 13, 2793–2825,, 2013. 

Keller, D. P., Lenton, A., Scott, V., Vaughan, N. E., Bauer, N., Ji, D., Jones, C. D., Kravitz, B., Muri, H., and Zickfeld, K.: The Carbon Dioxide Removal Model Intercomparison Project (CDRMIP): rationale and experimental protocol for CMIP6, Geosci. Model Dev., 11, 1133–1160,, 2018. 

Krasting, J. P., Dunne, J. P., Shevliakova, E., and Stouffer, R. J.: Trajectory sensitivity of the transient climate response to cumulative carbon emissions, Geophys. Res. Lett., 41, 2520–2527,, 2014. 

Le Quéré, C., Andrew, R. M., Friedlingstein, P., Sitch, S., Hauck, J., Pongratz, J., Pickers, P. A., Korsbakken, J. I., Peters, G. P., Canadell, J. G., Arneth, A., Arora, V. K., Barbero, L., Bastos, A., Bopp, L., Chevallier, F., Chini, L. P., Ciais, P., Doney, S. C., Gkritzalis, T., Goll, D. S., Harris, I., Haverd, V., Hoffman, F. M., Hoppema, M., Houghton, R. A., Hurtt, G., Ilyina, T., Jain, A. K., Johannessen, T., Jones, C. D., Kato, E., Keeling, R. F., Goldewijk, K. K., Landschützer, P., Lefèvre, N., Lienert, S., Liu, Z., Lombardozzi, D., Metzl, N., Munro, D. R., Nabel, J. E. M. S., Nakaoka, S., Neill, C., Olsen, A., Ono, T., Patra, P., Peregon, A., Peters, W., Peylin, P., Pfeil, B., Pierrot, D., Poulter, B., Rehder, G., Resplandy, L., Robertson, E., Rocher, M., Rödenbeck, C., Schuster, U., Schwinger, J., Séférian, R., Skjelvan, I., Steinhoff, T., Sutton, A., Tans, P. P., Tian, H., Tilbrook, B., Tubiello, F. N., van der Laan-Luijkx, I. T., van der Werf, G. R., Viovy, N., Walker, A. P., Wiltshire, A. J., Wright, R., Zaehle, S., and Zheng, B.: Global Carbon Budget 2018, Earth Syst. Sci. Data, 10, 2141–2194,, 2018. 

Lowe, J. A., Huntingford, C., Raper, S. C. B., Jones, C. D., Liddicoat, S. K., and Gohar, L. K.: How difficult is it to recover from dangerous levels of global warming?, Environ. Res. Lett., 4, 014012,, 2009. 

MacDougall, A. H.: The Transient Response to Cumulative CO2 Emissions: a Review, Curr. Clim. Change Reports, 2, 39–47,, 2016. 

MacDougall, A. H.: Limitations of the 1 % experiment as the benchmark idealized experiment for carbon cycle intercomparison in C4MIP, Geosci. Model Dev., 12, 597–611,, 2019. 

MacDougall, A. H. and Knutti, R.: Projecting the release of carbon from permafrost soils using a perturbed parameter ensemble modelling approach, Biogeosciences, 13, 2123–2136,, 2016. 

MacDougall, A. H., Zickfeld, K., Knutti, R., and Matthews, H. D.: Sensitivity of carbon budgets to permafrost carbon feedbacks and non-CO2 forcings, Environ. Res. Lett., 10, 125003,, 2015. 

Matthews, H. D. and Caldeira, K.: Stabilizing climate requires near-zero emissions, Geophys. Res. Lett., 35, L04705,, 2008. 

Matthews, H. D. and Solomon, S.: Irreversible Does Not Mean Unavoidable, Science, 80, 340,, 2013. 

Matthews, H. D. and Weaver, A. J.: Committed climate warming, Nat. Geosci., 3, 142,, 2010. 

Matthews, H. D. and Zickfeld, K.: Climate response to zeroed emissions of greenhouse gases and aerosols, Nat. Clim. Change, 2, 338–341,, 2012. 

Matthews, H. D., Gillett, N. P., Stott, P. A., and Zickfeld, K.: The proportionality of global warming to cumulative carbon emissions, Nature, 459, 829-U3,, 2009. 

Matthews, H. D., Landry, J. S., Partanen, A. I., Allen, M., Eby, M., Forster, P. M., Friedlingstein, P., and Zickfeld, K.: Estimating Carbon Budgets for Ambitious Climate Targets, Curr. Clim. Change Reports, 3, 69–77,, 2017. 

Mengis, N., Partanen, A.-I., Jalbert, J., and Matthews, H. D.: 1.5 C carbon budget dependent on carbon cycle uncertainty and future non-CO-2 forcing, Sci. Rep., 8, 5831,, 2018. 

Millar, R. J. and Friedlingstein, P.: The utility of the historical record for assessing the transient climate response to cumulative emissions, Philos. Trans. R. Soc. A, 376, 20160449,, 2018. 

Raupach, M. R., Canadell, J. G., Ciais, P., Friedlingstein, P., Rayner, P. J., and Trudinger, C. M.: The relationship between peak warming and cumulative CO2 emissions, and its use to quantify vulnerabilities in the carbon-climate-human system, Tellus, Ser. B Chem. Phys. Meteorol., 63, 145–164,, 2011. 

Rogelj, J., Hare, W., Lowe, J., van Vuuren, D. P., Riahi, K., Matthews, B., Hanaoka, T., Jiang, K., and Meinshausen, M.: Emission pathways consistent with a 2 C global temperature limit, Nat. Clim. Change, 1, 413–418, 2011. 

Rogelj, J., Meinshausen, M., Schaeffer, M., Knutti, R., and Riahi, K.: Impact of short-lived non-CO2 mitigation on carbon budgets for stabilizing global warming, Environ. Res. Lett., 10, 075001,, 2015. 

Rogelj, J., Shindell, D., Jiang, K., Fifita, S., Forster, P., Ginzburg, V., Handa, C., Kheshgi, H., Kobayashi, S., Kriegler, E., Mundaca, L., Séférian, R., and Vilariño, M. V.: Mitigation Pathways Compatible with 1.5 C in the Context of Sustainable Development, in: Global Warming of 1.5 C, An IPCC Special Report on the impacts of global warming of 1.5 C above pre-industrial levels and related global greenhouse gas emission pathways, in the context of strengthening the global response to the threat of climate change, edited by: Masson-Delmotte, V., Zhai, P., Pörtner, H.-O., Roberts, D., Skea, J., Shukla, P. R.,Pirani, A., Moufouma-Okia, W., Péan, C., Pidcock, R., Connors, S., Matthews, J. B. R., Chen, Y., Zhou, X., Gomis, M. I., Lonnoy, E., Maycock, T., Tignor, M., and Waterfield, T., 2018. 

Solomon, S., Plattner, G.-K., Knutti, R., and Friedlingstein, P.: Irreversible climate change due to carbon dioxide emissions, P. Natl. Acad. Sci. USA, 106, 1704–1709,, 2009. 

Steinacher, M. and Joos, F.: Transient Earth system responses to cumulative carbon dioxide emissions: linearities, uncertainties, and probabilities in an observation-constrained model ensemble, Biogeosciences, 13, 1071–1103,, 2016. 

Tachiiri, K., Hajima, T., and Kawamiya, M.: Increase of uncertainty in transient climate response to cumulative carbon emissions after stabilization of atmospheric CO2 concentration, Environ. Res. Lett., 10, 125018,, 2015.  

Tokarska, K. B., Gillett, N. P., Arora, V. K., Lee, W. G., and Zickfeld, K.: The influence of non-CO2 forcings on cumulative carbon emissions budgets, Environ. Res. Lett., 13, 034039,, 2018. 

Weaver, A. J., Eby, M., Wiebe, E. C., Bitz, C. M., Duffy, P. B., Ewen, T. L., Fanning, A. F., Holland, M. M., MacFadyen, A., Matthews, H. D., Meissner, K. J., Saenko, O., Schmittner, A., Wang, H. X., and Yoshimori, M.: The UVic Earth System Climate Model: Model description, climatology, and applications to past, present and future climates, Atmos.-Ocean, 39, 361–428, 2001. 

Zickfeld, K., Eby, M., Matthews, H. D., and Weaver, A. J.: Setting cumulative emissions targets to reduce the risk of dangerous climate change, P. Natl. Acad. Sci. USA, 106, 16129–16134,, 2009. 

Zickfeld, K., Eby, M., Weaver, A. J., Alexander, K., Crespin, E., Edwards, N. R., Eliseev, A. V., Feulner, G., Fichefet, T., Forest, C. E., Friedlingstein, P., Goosse, H., Holden, P. B., Joos, F., Kawamiya, M., Kicklighter, D., Kienert, H., Matsumoto, K., Mokhov, I. I., Monier, E., Olsen, S. M., Pedersen, J. O. P., Perrette, M., Philippon-Berthier, G., Ridgwell, A., Schlosser, A., Von Deimling, T. S., Shaffer, G., Sokolov, A., Spahni, R., Steinacher, M., Tachiiri, K., Tokos, K. S., Yoshimori, M., Zeng, N., and Zhao, F.: Long-Term climate change commitment and reversibility: An EMIC intercomparison, J. Climate, 26, 5782–5809,, 2013. 


The requested paper has a corresponding corrigendum published. Please read the corrigendum first before downloading the article.

Short summary
Global warming is simply related to the total emission of CO2 allowing us to define a carbon budget. However, information on the Zero Emissions Commitment is a key missing link to assess remaining carbon budgets to achieve the climate targets of the Paris Agreement. It was therefore decided that a small targeted MIP activity to fill this knowledge gap would be extremely valuable. This article formalises the experimental design alongside the other CMIP6 documentation papers.