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《JOURNAL OF GLACIOLGY AND GEOCRYOLOGY》 2000-01
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The Influence of ENSO Event on the Modern δ~(1 8)O on the Guliya Ice Core

ZHANG Xin-ping; YAO Tan-dong; JIN Hui-jun ( Territory Institute, Hunan Normal University, Changsha Hunan 410081. Chian ; Cold and Arid Regions Environmental and Engineering Research Institute, Lanzhou Gansu 730000, China )  
The relationships between the δ~(1 8)O in the Guliya ice core on the Tibetan Plateau and the SOI, as well as between the δ~(1 8)O and the SST in the eastern Equatorial Pacific are analyzed. In the E1 Nino years, no matter in midsummer or in midwinter, δ~(1 8)O in the Guliya ice core decreased, showing a marked decrease of temperature. The mean extents of the decrease were 1.2℃ and 0.45℃ respectively, and were 2.03℃ and 1.46℃ respectively in the strongest E1 Nino years; In the La Nina years, δ~(1 8)O in the Guliya ice core in midsummer increased, showing a marked rise of temperature. The mean extents of rising was 1.02℃, and was 1.6℃ in the strongest La Nina years. However, the va- nation of δ~(1 8)O in midwinter was undefined; In non-La Nina years, the linear correlation between δ~(1 8)O in midwinter and SOI in March of the corresponding period, as well as between and SST in January of the corresponding period became obvious.
【Fund】: 国家重点基础研究规划项目!G1998040802;; 国家攀登计划!KZ951-A1-204-02,KZ951-A1-402
【CateGory Index】: P343.6
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