Rib21.yaml

- key: Rib21 Constrained TCR
  doi: 10.1126/sciadv.abc0671
  metric:
    name: TCR
    long_name: Transient Climate Response
    units: K
    variables: tas
    comment: >
      TCR is calculated from the CO2-only simulation, where the atmospheric CO2
      concentration increases at a rate of 1% per year, centered on the time of
      doubling of the atmospheric CO2, which occurs during simulation year 70
      (we use the mean of the years 61 to 80).

      The values of the GCM TCR  can be found in Suppl. Mat Table S1. Some model
      TCR are missing. This study is based on multi-member for each model, not
      on only one member.
  type: performance
  spatial_scope: Global
  temporal_scope: Annual
  period:
    reference: 1850-2019
    comment: >
      This is not the period for the metric values (these are model years at
      the time of doubling CO2), but the one used in the observational constraint.
  plausible_values:
    min: 1.33
    max: 2.36
    source: reference
    comment: >
      This is a 90% likely range (5-95%) for the TCR.
      HadCRUT4-CW (Cowtan & Way, 2014) used as observational reference.
  data_source: reference
  data:
    BCC-CSM2-MR_r1i1p1f1: 1.6
    CanESM5_r1-3i1p2f1: 2.75
    CESM2_r2i1p1f1: 1.99
    CNRM-CM6-1_r1i1p1f2: 2.23
    CNRM-CM6-1-HR_r1i1p1f2: 2.47
    CNRM-ESM2-1_r1i1p1f2: 1.82
    EC-Earth3_r1i1p1f1: 2.32
    EC-Earth3-Veg_r1-3i1p1f1: 2.76
    GFDL-ESM4_r1i1p1f1: 1.61
    INM-CM5-0_r1i1p1f1: 1.39
    IPSL-CM6A-LR_r1-6i1p1f1: 2.39
    IPSL-CM6A-LR_r14i1p1f1: 2.39
    MIROC6_r1i1p1f1: 1.58
    MPI-ESM1-2-HR_r1i1p1f1: 1.57
    MRI-ESM2-0_r1i1p1f1: 1.67
    NESM3_r1i1p1f1: 2.79
    NorESM2-LM_r1i1p1f1: 1.48
    NorESM2-MM_r1i1p1f1: 1.48
    UKESM1-0-LL_r1-3i1p1f2: 2.79