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Local and Regional Indian Summer Monsoon Precipitation Dynamics During Termination II and the Last Interglacial
Abstract To date Indian summer monsoon (ISM) dynamics have been assessed by changes in stalagmite δ 18 O. However, stalagmite δ 18 O is influenced by multiple environmental factors (e.g., atmospheric moisture transport, rainfall amount at the study site, and ISM seasonality), precluding simple and
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