River floods are among the deadliest natural hazards worldwide. Substantial increases in economic damage from disastrous floods have raised demands for improved understandings of flood changes in terms of magnitude, frequency, and timing (e.g., Merz et al., 2021;Tellman et al., 2021). This is particularly a critical issue for East Asia, where more than two-thirds of global future flood losses occur and more than half of the future population will be affected by floods (Dottori et al., 2018). The dominance of monsoon climate also makes East Asian countries important places to investigate whether there are consistent regional changes of river floods under a changing climate (Blöschl et al., 2017;Hall et al., 2014), but such investigations are still limited.Compared to magnitude, flood peak timing is relatively less affected by water (e.g., reservoirs) and land management practices (e.g., urbanization) (Blöschl et al., 2017;Villarini, 2016), and is preferably adopted to understand changes of river floods under a changing climate (