“…The year‐to‐year variation in Meiyu rainfall depends not only on the El Niño–Southern Oscillation (ENSO) and its resultant SST anomaly in the Indian Ocean (Kosaka et al, 2011; B. Wang et al, 2013) but also on the middle‐high‐latitude wave trains over the Eurasian continent (H. Hsu & Lin, 2007; Liu, Ke, & Ding, 2019; Z. Wang et al, 2018). On a subseasonal timescale, the intraseasonal oscillation (ISO) of the EASM is most crucial for Meiyu activity (Ding et al, 2020; Huang et al, 2019; Lau et al, 1988; Li et al, 2015; Song et al, 2016; B. Wang & Xu, 1997; C. Zhu et al, 2003). Moreover, the subseasonal variation of Meiyu rainfall is modulated by the Madden‐Julian Oscillation (MJO) (X. Li et al, 2018) or the summer North Atlantic Oscillation (NAO) (Bollasina & Messori, 2018).…”