Abstract
The local meteoric water line (MWL) has been established from north to south of the Tibetan Plateau based on the measured results of δ D and δ 18 O in precipitation and river water, and the relationship between MWL and moisture origins discussed. The spatial and seasonal variations of d in precipitation and river water on the Tibetan Plateau have been studied. Results show that the spatial and seasonal variations of d between north and south of the Tanggula Mountains are related to different moisture origins and water recycling.
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