A high-resolution ice core record from Dasuopu, Tibet, reveals that this si
te is sensitive to fluctuations in the intensity of the South Asian Monsoon
. Reductions in monsoonal intensity are recorded by dust and chloride conce
ntrations. The deeper, older sections of the Dasuopu cores suggest many oth
er periods of drought in this region, but none have been of greater intensi
ty than the greatest recorded drought, during 1790 to 1796 A.D. of the Last
millennium. The 20th century increase in anthropogenic activity in India a
nd Nepal, upwind from this site, is recorded by a doubling of chloride conc
entrations anti a fourfold increase in dust. Like other ice cores from the
Tibetan Plateau, Dasuopu suggests a Large-scale, plateau-wide 20th-century
warming trend that apl,ears to be amplified at higher elevations.