DOI: 10.5281/zenodo.10566646
title: FaIR calibration data

description: This dataset contains the full data, input scripts and produced output data for the AR6-consistent calibration of FaIRv2.1.3.

The zipfile contains everything, allowing you perform your own analysis. The GitHub version contains enough for "bare bones" reproducibility, including downloading of external datasets and generation of intermediate files. 

Two CSV files of the constrained parameter set and the chemical sensitivies to methane lifetime are provided. This may be all that is required to run your own simulations without dipping into the ZIP file.

FaIR v2.1.3

Obtainable from https://pypi.org/project/fair/

From the command line:

pip install fair==2.1.3

Calibration v1.4

A slightly bigger prior and slightly smaller posterior are implemented. ERFari distributions are changed to bring them closer in line with the intent of AR6 WG1 Ch6. ERFaci prior is made slightly wider and non-uniform. Contrails are excluded from the calibration since few IAM scenarios provide detailed enough information to assess their future forcing (some kind of aviation activity indicator or proxy such as emissions from the sector would be needed).



1.6 million prior ensemble

Climate response calibrated on 49 abrupt-4xCO2 experiments from CMIP6 and sampled using correlated kernel density estimates

Methane lifetime calibrated on 4 AerChemMIP experiments for 1850 and 2014 (Thornhill et al. 2021a, 2021b). Unlike other variables which are sampled around some prior uncertainty, only the best estimate historical calibration is used. The base (1750) lifetime has been fixed and consistently used across projections.

Carbon cycle uses the parameters from Leach et al. 2021 calibrated for FaIR 2.0.0 using 11 C4MIP models.

Aerosol cloud interactions depend on SO2, BC and OC, using new calibrations from 13 RFMIP and AerChemMIP models, with the APRP code fixed by Mark Zelinka (Zelinka et al. 2023). Prior is a trapezoidal distribution with vertices at (-2.2, -1.6, -0.4, +0.2) W/m2.

Aerosol radiation interactions use prior values from AR6 Ch6, with best estimates and uncertainties scaled to create a prior in the range of -0.6 to 0.0 W/m2.

Ozone uses the same methodology as AR6 (Smith et al. 2021b).

NOx emissions are updated from RCMIP to fix a unit conversion issue, where biomass burning emissions from GFED are in units of NO and everything else (from CEDS) is in NO2. FaIR uses NO2 units consistently. In RCMIP v5.1.0 (Nicholls and Lewis 2021), the conversion was not done. When using this calibration for future scenarios, it is important that this is carefully considered.

Effective radaitive forcing uncertainty follows the distributions in AR6, with asymmetric distributions switched to skew-normal.

Volcanic forcing time series updated to 2022 (from IGCC).

Contrails are excluded from the calibration


AR6-updated_no-contrails (v1.4.0)



841-member posterior (deliberately chosen).

Emissions and concentrations from RCMIP (i.e. based on CMIP6), but with NOx updated as above. ssp245 chosen for post-2014.

Temperature from IGCC (Forster et al. 2023) (1850-2022, mean of 4 datasets).

Warming 2003-2022 relative to 1850-1900 range from IGCC.

CO2 concentrations constrained to IGCC estimate for 2022.

Ocean heat content from IGCC (1971-2020), linear.

two step constraining procedure used: first RMSE of less than 0.17K (up from 0.16), then 8-variable distribution fitting.

Aerosol ERF, ERFari and ERFaci as in AR6 WG1

No future warming constraints


Performance relative to AR6 assessed ranges

On request, as Zenodo seems to have removed the ability to format tables in the dataset description.

References



Forster et al. 2023: https://doi.org/10.5194/essd-15-2295-2023

Leach et al. 2021: https://doi.org/10.5194/gmd-14-3007-2021

Nicholls and Lewis 2021: https://doi.org/10.5281/zenodo.4589756

Smith et al. 2021a: https://doi.org/10.1029/2020JD033622

Smith et al. 2021b: https://www.ipcc.ch/report/ar6/wg1/downloads/report/IPCC_AR6_WGI_FGD_Chapter07_SM.pdf

Thornhill et al. 2021a: https://doi.org/10.5194/acp-21-853-2021

Thornhill et al. 2021b: https://doi.org/10.5194/acp-21-1105-2021

Zelinka et al. 2023: https://doi.org/10.5194/acp-23-8879-2023