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| The δ~(18)O in the Guliya shallow ice core during the prevailing summer monsoons and sea-air interactions | |
| 作者姓名： | ZHANG Xin-ping Masayoshi Nakawo YAO Tan-dong (. Nanjing Institute of Geography and Limnology CAS Nanjing Chin . Institute of Territory and Environment Research Hunan Normal University Changsh Chin . Institute for Hydro |
| 作者单位： | 1. Nanjing Institute of Geography and Limnology，CAS，Nanjing 210008，China; 2. Institute of Territory and Environment Research，Hunan Normal University，Changsha 410081，China; 3. Institute for Hydro |
| 基金项目： | Under the auspices of the G1998040802，BX2001-03 and KXCX2-301 programs |
| 摘 要： | 1 Introduction The Tibetan Plateau is gigantic in extent and has the highest elevation and the most complex topography in the world. Its existence is of important significance for the formation of atmospheric circulation, weather and climate in China, much of Asia and even of the globe. Therefore, great attention is given to it. The analyses show that the influencing range of the Tibetan Plateau is the widest during the summer[1]. The powerful updrafts from the plateau warm low flow towar… |
| 关 键 词： | the Tibetan Plateau the Guliya ice core δ18Omax SST circulation at 500 hPa correlation |
| 本文献已被 CNKI 等数据库收录！ | |