The temporal and spatial variations of the δ~18O in precipitation on the Tibetan plateau are analyzed. There is no temperature effect in the southern Tibetan Plateau. Amount effet has been observed at Lhasa station. However, the seasonal variations of the δ~18O in precipitation are different from that of precipitation intensity, showing that the precipitation intensity is not a main controlling factor on the stable isotopic compositions in precipitation in the southern Tibetan Pla- Teau.
展开▼
