“…The criteria for proxy selection are (a): The data developer utilized the proxy record to characterize EASM variability; (b) the indicators can capture the EASM variability or precipitation variability; (c) the timespan of the proxy record exceeds 100 years, and it covers the 1880–1998 CE initial calculation period; (d) the temporal resolution of the proxy record is less than 10 years or better. We screened 23 proxy records including 2 tree ring width chronologies (Sun et al., 2021; Yang et al., 2014) and 10 tree ring δ 18 O chronologies (Liu, Cobb, et al., 2017; Liu, Wang, et al., 2019; Nakatsuka et al., 2020; Sano et al., 2012; Seo et al., 2019; Xu, Sano, et al., 2013; Xu, Zheng, et al., 2013; Xu et al., 2015; Xu et al., 2016; Yang et al., 2021), 7 speleothem δ 18 O records (Cai et al., 2010; Hu et al., 2008; Tan et al., 2010, 2018, 2020; Wang et al., 2005; Zhang et al., 2008), and 4 historical documentary records (Ge et al., 2008; Mizukoshi, 1993; Shi, Zhao, et al., 2017; Wang et al., 2021) (Figure 3). The historical documentary records are in the monsoon core area, and the natural proxy records are mainly distributed in the monsoon fringe area.…”