Skip to main content
. 2024 Aug 12;15:6889. doi: 10.1038/s41467-024-50874-0

Table 1.

Characteristics of the 16 CMIP6 models used in this study: horizontal resolution in the Arctic, atmospheric model component, ocean model component, sea ice model component, ice-ocean drag coefficient, and reference

Model Resolution Atmospheric model Ocean model Sea ice model 10−3Cw Reference
CAMS-CSM1-0 54 km ECHAM5-CAMS MOM41 SIS1.0 3.24 68
CanESM5 50 km CanEM5 NEMO3.4.1 LIM2 5.0 69
CESM2 41 km CAM6 POP2 CICE5 5.36 70
CMCC-ESM2 49 km CAM5.4 NEMO3.6 CICE4 n/a 71
CNRM-CM6-1 49 km ARPEGE NEMO3.6 GELATO 10 72
EC-Earth3 49 km IFS 36r4 NEMO3.6 LIM3 5.0 73
FIO-ESM-2-0 50 km CAM5 POP2 CICE4 5.36 74
GFDL-CM4 9 km AM4 MOM6 SIS2 3.24 75
GFDL-ESM4 18 km AM4 MOM6 SIS2 3.24 76
HadGEM3-GC31-LL 49 km GA7 NEMO3.6 CICE5.1 10 77
IPSL-CM6A-LR 49 km LMDZ6A NEMO3.2 LIM3.6 5.0 78
MIROC6 39 km AGM COCO4.9 COCO4.9 20 79
MPI-ESM1-2-HR 36 km ECHAM6.3 MPIOM1.63 MPIOM1.63 4.5 80
MRI-ESM2-0 39 km MRIAGCM3.5 MRI.COMv4 MRI.COMv4 5.5 81
NorESM2-MM 38 km CAM6-Nor BLOM (MICOM) CICE5 5.36 29
UKESM1-0-LL 50 km MetUM-GA7 NEMO3.6 CICE5 n/a 82

The horizontal resolution in the Arctic (2nd column) was calculated as the square root of the total area north of 70N divided by the number of points the model has north of 70N. Parameters used in this study include: tauuo, tauvo, siconc, sithick, sivol, siv, siu, sfcwind, tauu, tauv, siforceinstrx, siforceinstry, sistrxdtop, sistrxubot, sistrydtop, sistryubot, tas, psl, uo, and vo. All models employ a constant ice-ocean drag coefficient Cw, with values given above.