Table 3.
Mean climatological differences.
| Tmax | Tmin | RHave | ||||
|---|---|---|---|---|---|---|
| GSOD - CHC-CMIP6 | GSOD - raw CMIP6 | GSOD - CHC-CMIP6 | GSOD - raw CMIP6 | GSOD - CHC-CMIP6 | GSOD - raw CMIP6 | |
| Global | −0.08 | 1.45 | −2.21 | −0.91 | 4.43 | −0.68 |
| Africa | −0.13 | 1.12 | −2.23 | −0.36 | 3.71 | 0.8 |
| Asia | −0.16 | 1.98 | −1.86 | 0.1 | 4.62 | −0.14 |
| Europe | −0.31 | 1.48 | −1.83 | −0.52 | 4.82 | 1.88 |
| North America | 0.32 | 1.63 | −2.11 | −1.45 | 4.43 | −2.37 |
| Oceania | −0.57 | 1.08 | −3.42 | −2.54 | 6.14 | −2.16 |
| South America | 0.35 | 1.4 | −1.8 | −0.68 | 2.89 | −2.08 |
Table depicts mean bias. Bias refers to climatological GSOD minus CHC-CMIP6 versus GSOD minus raw CMIP6 for the local hottest month. CHC-CMIP6 and raw CMIP6 biases are significantly different from each other (Mann-Whitney p-value < 0.01). Global averaged climatological Tmax is similar for GSOD and CHC-CMIP6 (0.08 °C difference), yet CMIP6 Tmax presents a cool bias (1.59 °C), while less present for Tmin. This indicates that the projected CHC-CMIP6 fields likely contain a cool bias.