| Relationships between δ ~(18)O in summer precipitation and temperature and moisture trajectories at Muztagata, western China |
| |
| 作者单位： | YU Wusheng1，2，YAO Tandong1，2，TIAN Lide1，2，LI Zhen2，SUN Weizhen2 & WANG Yu2 1. Laboratory of Environment and Process on Tibetan Plateau，Institute of Tibetan Plateau Research，Chinese Academy of Sciences，Beijing 100085，China; 2. Key Laboratory of Cryosphere and Environment，Jointly Established by Cold and Arid Regions Environmental and Engi-neering Research Institute and Institute of Tibetan Plateau Research，Chinese Academy of Sciences and Chinese Academy of Meteorological Sciences，China Meteorological Administration，CAS，Lanzhou 730000，China |
| |
| 摘 要： | Stable isotopes are widely used to reconstruct pa-leoclimate variations preserved in ice core records. However, the interpretation of stable isotope records in ice cores must be based on the knowledge of temporal and spatial variations of stable isotopes …
|
| 关 键 词： | Muztagata δ 18O precipitation temperature moisture transport. |
| 本文献已被 CNKI 等数据库收录！ |
