“…Variations in total solar irradiance (TSI) are an important driver of climate system changes (Beer et al., 2000), including terrestrial climate (J. Wang et al., 2023). The coherence between ASM intensity and solar variability on multidecadal to centennial timescales has previously been recognized in paleoclimate records; accordingly, previous high‐resolution paleoclimate studies have suggested TSI as one of the primary controls on Asian monsoon intensity (Neff et al., 2001; Tiwari et al., 2005; Y. Wang et al., 2005; J. Zhang et al., 2021). Oxygen isotope records from Dongge Cave suggest stronger EASM intensity corresponds to higher TSI over the Holocene (Y. Wang et al., 2005), whereas increased rainfall corresponding to weakened solar irradiance has been reported from mid‐Yangtze River Valley (YRV) over the past two millennia (J. Zhang et al., 2021).…”