Table 2 Overview of the CMIP6 ensemble of GCMs used as initial and boundary conditions for the downscaling process.
From: High-resolution regional climate projections and tourism impacts in the Macaronesian archipelagos
GCM | Institution(s) (country) | Horizontal resolution | References |
|---|---|---|---|
ACCESS-ESM1-5 | CSIRO and BOM (Australia) | \(1.875^{\circ }\times 1.25^{\circ }\) | Mackallah et al.38 |
AWI-CM-1-1-MR | AWI (Germany) | \(\approx 0.9^{\circ }\times 0.9^{\circ }\) | Semmler et al.39 |
BCC-ESM2-MR | BCC (China) | \(1.1^{\circ }\times 1.1^{\circ }\) | Wu et al.40 |
CanESM5 | CCCma (Canada) | \(\approx 2.8^{\circ }\times 2.8^{\circ }\) | Swart et al.41 |
CESM2 | NCAR (USA) | \(1.25^{\circ }\times 0.9^{\circ }\) | Danabasoglu et al.42 |
CMCC-ESM2 | CMCC (Italy) | \(2.5^{\circ }\times 1.25^{\circ }\) | Lovato et al.43 |
EC-Earth3 | EC-Earth Consortium (Europe) | \(\approx 0.7^{\circ }\times 0.7^{\circ }\) | Döscher et al.44 |
FGOALS-g3 | CAS (China) | \(2^{\circ }\times 2.3^{\circ }\) | Li et al.45 |
GFDL-ESM4 | GFDL (USA) | \(\approx 1^{\circ }\times 1^{\circ }\) | Krasting et al.46 |
GISS-E2-1-GN | GISS (USA) | \(2.5^{\circ }\times 2^{\circ }\) | Kelley et al.47 |
INM-CM5-0 | INM (Russia) | \(2^{\circ }\times 1.5^{\circ }\) | Volodin et al.48 |
IPSL-CM6A-LR | IPSL (France) | \(2.5^{\circ }\times 1.25^{\circ }\) | Boucher et al.49 |
MIROC6 | JAMSTEC, AORI, NIES, R-CCS (Japan) | \(1.4^{\circ }\times 1.4^{\circ }\) | Tatebe et al.50 |
MPI-ESM1-2-HR | MPI-M (Germany) | \(\approx 0.9^{\circ }\times 0.9^{\circ }\) | Jungclaus et al.51 |
MRI-ESM2-0 | MRI (Japan) | \(1.1^{\circ }\times 1.1^{\circ }\) | Yukimoto et al.52 |
NorESM2-MM | NCC (Norway) | \(1.25^{\circ }\times 0.9^{\circ }\) | Selend et al.53 |
TaiESM1 | AS-RCEC (Taiwan) | \(1.25^{\circ }\times 0.9^{\circ }\) | Lee et al.54 |
