Mass?Wasting?Inferred Dramatic Variability of 130,000?Year Indian Summer Monsoon Intensity From Deposits in the Southeast Tibetan Plateau

A large proportion (?80%) of the Indian subcontinent's precipitation comes from summer monsoon (ISM), which influences one-fifth world's population. long-term reliable proxy for ISM is fundamental to understanding previous global climate change. We establish a mass-wasting-inferred examine paleo-hydrogeology (river undercutting history) Southeast Tibetan Plateau and reconstruct dramatic variability intensity (precipitation) in past 130,000 years. Our data suggest that mass-wasting events, provides us sufficient samples paleoclimate research, are prone changes, especially extreme environments. The was subjected at least four distinct phases conclude has cyclicity featured by Earth's orbit with obliquity, transition lags ice volume (sea level) change 8–15 kyrs.