“…It is also believed that atmospheric circulation plays a role in influencing the variability of precipitation isotopes by governing changes of moisture sources and by affecting temperatures, pressures, and humidity conditions experienced by advecting moisture masses (e.g., Aggarwal, Fröhlich, Kulkarni, & Gourcy, ; Cole, Rind, Webb, Jouzel, & Healy, ; Tan, ; Tian et al, ). Such large‐scale circulation effects may be El Niño–Southern Oscillation and summer monsoon activities (e.g., Ichiyanagi & Yamanaka, ; Tan, ; Vuille et al, ), westerly circulation (e.g., X. Liu, Rao et al, ), North Atlantic Oscillation (e.g., Baldini, McDermott, Foley, & Baldini, ; Mischel, Scholz, & Spötl, ) and Arctic Vortex (e.g., Puntsag et al, ). Although these analyses contribute significantly to our understanding of how isotopic signals are influenced by various factors, most analyses, however, tend to reveal a combined effect of moisture sources and meteorological parameters, as they are usually based on monthly samples with integrated precipitation from different moisture sources or even‐based data without considering the influence of various moisture sources.…”