Compound heatwave–pluvial events (CHPEs)—heatwaves followed by heavy rain within 7 days—are rising worldwide.
1980–2021 saw more and longer CHPEs, with hotspots in Central Europe, East Asia and North America.
Sensible heat flux (SSHF) and total column water vapor (TCWV) promote heatwave-to-pluvial shifts.
Under Shared Socioeconomic Pathway 5-8.5 (SSP5-8.5), exposure rises fastest in low-income countries.
Targeted mitigation and adaptation are needed to protect dense urban hotspots and reduce climate inequality.
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Spatial characteristics of compound heatwave-pluvial events (CHPEs) from 1980 to 2021
Trends in CHPEs frequency and duration (1980–2021)
Influence of five hydroclimatic anomalies on the risk of occurrence of CHPEs (including surface sensible heat flux [SSHF], specific humidity [SH], total column water vapor [TCWV], convective available potential energy [CAPE], and vertically integrated moisture converge [VIMC])
Distributions of odds ratios across 1–7-day lags
Spatiotemporal characteristics of population and GDP exposure to CHPEs from 1980 to 2021
Temporal changes in the global average proportion for exposed population and GDP under SSP5-8.5
Changes in population (A) and GDP exposure (B) in the future (2021–