Supplemental Material: Asynchronous Holocene lake evolution in arid mid-latitude Asia is driven by glacial meltwater and variations in Westerlies and the East Asian summer monsoon

This document presents details on luminescence dating sample preparation, analytical facilities (Supplemental Text S1) and quartz and K-feldspar luminescence dating measurement, and dose rate determination (Supplemental Text S2), the photograph, locational information and luminescence dating results of the paleoshorelines at Aibi Lake Basin (Figures S1-S4 and Table S1-S6), and the reconstructed lake area changes of Aibi Lake during past 18 ka (Figure S5).