稳定氧同位素(δ^18O)在冰芯研究中能够很好地反映气候变化,尤其是气温变化的一项重要指标。研究青藏高原降水中8墟。为科学的解释冰芯中δ^18O。记录具有重要的指示意义。分别介绍了青藏高原季风区、非季风区以及季风区知非季风区的过渡区降水中δ^18O研究历史和现状,并对该领域未来的研究趋势进行了展望。
Stable oxygen isotope (δ^18O) in ice core records is good proxy for temperature record and is representative of climatic change. The study of the δ^18O variation in precipitation can throw light on the climatic significance of δ^18O records in ice core. This paper reviews the advances in the study of stable oxygen isotope in precipi- tation in the monsoon region, the non-monsoon region, and the transition region between the monsoon region and the non-monsoon region on the Tibetan Plateau, respectively. Moreover, an outlook on future research over the Tibetan Plateau is presented in this paper.