Abstract Temperature and precipitation variability in monsoonal Asia is central to understanding regional climate dynamics and global teleconnections. How post‐LGM warming and hydroclimate change unfolded in Northeast Asia, and how they were linked to external forcing, remain poorly constrained. Here we present high‐resolution pollen‐derived reconstructions of mean annual temperature (MAT) and precipitation (MAP) from Xiaolongwan Maar Lake, spanning the Last Glacial Maximum (LGM) to the present. From the LGM to the mid‐Holocene, MAT increased by ∼9.0 ± 2.2°C and MAP by ∼470 ± 121 mm. During ∼1
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