NDLI: Relation between stable isotope in monsoon precipitation in southern Tibetan Plateau and moisture transport history

Content Provider	Springer Nature Link
Author	Tian, Lide Yao, Tandong A., Numaguti Duan, Keqin
Copyright Year	2001
Abstract	The moisture transport history to the south of the Tibetan Plateau was modeled using the meteorological data provided by NCEP in this paper, and the modeled results were compared with the measured δ$^{18}$O in the south of the Tibetan Plateau. The relation between δ$^{18}$O in precipitation in the south of the Tibetan Plateau and moisture trajectories was discussed. The results show that the extremely low δ$^{18}$O in precipitation in the south of the Tibetan Plateau is always related to the moisture from the low-level sea surface evaporation. The long-distance transport of moisture also contributes to low δ$^{18}$O in precipitation probably due to the rainout process during moisture transport. It is also found that low δ$^{18}$O in precipitation is also related with deep layer transport of moisture, and with intensive condensation in the upper layers of the atmosphere, resulting in low δ$^{18}$O because of depletion of heavy isotopes in deep condensation. However, high δ$^{18}$O in precipitation whether in monsoon period or not is always companied with moisture coming from the upper layers, and the moisture is from northern or western sides of the plateau. The interpretation of the modeled results is in agreement with the isotope fractionation processes.
Starting Page	267
Ending Page	274
Page Count	8
File Format	PDF
ISSN	10069313
Journal	Science in China Series D: Earth Sciences
Volume Number	44
Issue Number	1
e-ISSN	18622801
Language	English
Publisher	Science in China Press
Publisher Date	2001-01-01
Publisher Place	Beijing
Access Restriction	Subscribed
Subject Keyword	stable isotope moisture transport processes south of the Tibetan Plateau Geosciences
Content Type	Text
Resource Type	Article
Subject	Earth and Planetary Sciences

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