“…Park & Jeong, 2022; C. Yin et al., 2022) and precipitation or fluvial flooding (Alfieri et al., 2017; H. Chen & Sun, 2021; Hirabayashi et al., 2013; Yamazaki et al., 2018) under different scenarios based on general circulation model (GCM) simulations (mainly Coupled Model Intercomparison Project Phase 6 [CMIP6] data) at the global scale. Moreover, regional‐scale studies have been carried out in areas with high vulnerability and dense populations such as South Asia (SAS) (Kumar & Mishra, 2020; Zhao et al., 2021), East Asia (EAS) (W. Zhang & Zhou, 2020), North America (Jones et al., 2015; Swain et al., 2020), and Africa (Fotso‐Nguemo et al., 2023; Iyakaremye et al., 2021). Considering that isolated studies of individual hazards performed through climate risk assessment may underestimate the amplifying effects of multiple extreme event combinations, some studies have been conducted to explore population exposure to compound events (AghaKouchak et al., 2020; Das et al., 2022; Raymond et al., 2020; Ridder et al., 2022; Wang et al., 2020; J. Yin et al., 2023; G. Zhang et al., 2022; Zscheischler et al., 2018), suggesting that under the impact of climate change, increasing numbers of people will be affected by different climate extremes, even compound events.…”