Summer monsoon variability in the himalaya over recent centuries

Masaki Sano*, Chenxi Xu, A. P. Dimri, R. Ramesh


研究成果: Chapter

4 被引用数 (Scopus)


Hydroclimatic variations during the summer monsoon season (June–September) across the Himalaya are examined over the past several hundred years using tree-ring oxygen isotope records. Owing to their strong associations with hydroclimatic variables including precipitation, relative humidity, and the Palmer Drought Severity Index, tree-ring δ18O chronologies from the Himalaya can be used to reconstruct summer monsoon intensity precisely. A regional chronology derived from five local chronologies across the Himalaya shows a significant correlation with Indian summer rainfall data. One of the most noteworthy features of the regional chronology is a drying trend over the past 180 years, indicating that summer monsoon intensity in the Himalayan region has weakened. A declining land–ocean thermal gradient over South Asia seems to be responsible for the weakened summer monsoon. By analyzing spatio-temporal correlations between zonally distributed tree-ring data over the Himalaya, we also explore possible changes in the relative contributions of source water originating in the Arabian Sea and the Bay of Bengal.

ホスト出版物のタイトルHimalayan Weather and Climate and their Impact on the Environment
出版社Springer International Publishing
出版ステータスPublished - 2019 1月 1

ASJC Scopus subject areas

  • 地球惑星科学(全般)
  • 環境科学(全般)
  • 農業および生物科学(全般)


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