In our study (1) we reconstructed the last 45 y of glacial evolution in the Southeastern Tibetan Plateau and revealed that decadal changes in spring and monsoon precipitation have respectively… Click to show full abstract
In our study (1) we reconstructed the last 45 y of glacial evolution in the Southeastern Tibetan Plateau and revealed that decadal changes in spring and monsoon precipitation have respectively mitigated and accentuated glacier mass losses. The mesoscale perspective of changes to atmos - pheric circulation and moisture supply described by Yang et al. (2) brings a timely explanation to the decrease in monsoon precipitation noticed by both studies since the early 2000s. Variations in
               
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