Isotopic variation in the lake water balance at the Yamdruk-tso basin, southern Tibetan Plateau
2008
Tian, Lide | Liu, Zhongfang | Gong, Tongliang | Yin, Changliang | Yu, Wusheng | Yao, Tandong
The use of stable isotopes is a practical tool in the study of the lake water budget. This is an one way to study the hydrological cycle in the large numbers of inland lakes on the Tibetan Plateau, in which the isotope record of the sediment is believed to reflect the climatic and environmental changes. The monitoring of stable isotopes of the precipitation, river and lake waters during 2004 in the inland Yamdruk-tso basin, southern Tibetan Plateau, reveals the lake water δ¹⁸O is over 10[per thousand] higher than the local precipitation. This high difference indicates strong isotope enrichment due to lake water evaporation. The simulation results based on the isotope technique show that the present lake water δ¹⁸O level corresponds to an average relative humidity of around 54-58% during evaporation, which is very close to the instrumental observation. The simulation results also show that the inland lakes on the Tibetan Plateau have a strong adjustability to the isotope shift of input water δ¹⁸O. On average, the isotope component in the inland lake water is to a large extent controlled by the local relative humidity, and can also be impacted by a shift of the local precipitation isotope component. This is probably responsible for the large consistence in the isotope component in the extensive inland lakes on the Tibetan Plateau.
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