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Stable isotopes in monsoon precipitation and water vapour in Nagqu, Tibet, and their implications for monsoon moisture
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文摘

Stable isotope signals change rapidly between the pre-monsoon and monsoon seasons.

Moisture sources vary through mixing of advected moisture with local recycling.

Both “temperature effect” and “amount effect” occurs in the transition zones.

High frequency stable isotopic data show “amount effect” in night-time rainfall.

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