Fig. 2: Extreme precipitation sensitivity (EPS) based on ERA5 and CMIP6 during the reference 1985–2014 period.
From: Large anomalies in future extreme precipitation sensitivity driven by atmospheric dynamics
a, b 99th-percentile precipitation-temperature scaling rate based on ERA5 reanalysis before Tpp (<Tpp, exhibiting three EPS regimes) and after the Tpp (>Tpp, i.e., only the decreasing branch in the hook-like scaling). c, d Results based on CMIP6 average multi-model ensemble experiments. Monotonic scaling types (monotonically increasing and decreasing regimes) in (b, d) are masked in grey.
