Stable isotope variations in monsoon precipitation on the Tibetan Plateau

Precipitation samples were collected in a large-scale region (more than 2,0 00 km from the north to the south of the Tibetan Plateau) and a middle scal e region (with an area about 9,000 km(2)) in the Tibetan Plateau to study t he impact of monsoon precipitation on stable isotopes. In the large-scale r egion, samples of precipitation and river water were collected at several s tations from the north to the south along the Qinghai-Tibet Highway on the plateau. Results show that the Indian monsoon not only influences the spati al variation of stable isotope in precipitation, but also the relationship between delta O-18 and deltaD. Deuterium excess (d) in areas where precipit ation is directly controlled by monsoon precipitation is lower, while in th e northern Tibetan Plateau, d is in higher value due to the influence of co ntinental air mass and strong local hydrological recycling. A detailed stud y on oxygen stal le isotope in precipitation was carried out on the middle scale in the Nagqu Basin area. The temporal variation of delta O-18 in dail y precipitation at 6 sites shows quite similar trends, indicating that delt a O-18 in precipitation in the middle Tibetan Plateau is mainly controlled by large-scale synoptic condition, rather than the local meteorological fac tors. The spatial variation of delta O-18 in precipitation in the basin agr ees with the Tibet-scale spatial variation trend and local hydrological rec ycling. Temporal variations of delta O-18 in precipitation also show a clos e relation to the movements of monsoon precipitation. The onset of monsoon in the earlier summer leads to low delta O-18 value. There is a negative re lation between delta O-18 and SWI (south wind index). High SWI, which repre sents intensive transport of moisture from south with the monsoon movement, is coincided with lower delta O-18 values, while low SWI, which represents moisture from inland air mass or local evaporated moisture, is associated with higher delta O-18 values.