“…They are generally detected based on the associated integrated vapor transport (IVT), which is the column integral of the flux of water vapor carried by the horizontal wind flow (Guan & Waliser, 2015; Guan et al., 2023; Lora et al., 2020; Zhou et al., 2018), while their strength and impacts are typically a function of the magnitude and persistence of high IVT values (Eiras‐Barca et al., 2021; Esfandiari & Rezaei, 2022; Ralph et al., 2019). ARs are associated with different time‐scales, ranging from high‐frequency (<10 days) predominantly over the mid‐latitude storm tracks, to low‐frequency in the summer monsoon regions, with intermediate ARs found on the poleward side of subtropical highs (Park et al., 2023). While in monsoon and lower latitude regions they further exacerbate rainfall events (Liang & Yong, 2021; Park et al., 2021; Vallejo‐Bernal et al., 2023; Yang et al., 2018), at high‐latitudes and over the high‐terrain, ARs can have a substantial effect on sea‐/land‐ice and snow cover (Box et al., 2023; Bozkurt et al., 2021; Fonseca et al., 2023; Francis et al., 2020, 2021a, 2022a, 2022b; Meinander et al., 2023; Shields et al., 2022b; Wille et al., 2024a, 2024b; Zhang et al., 2023).…”