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The δ^(18)O in the Guliya shallow ice core during the prevailing summer monsoons and sea-air interactions
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作者 ZHANG Xin-ping1,2, Masayoshi Nakawo3, YAO Tan-dong4 (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 《Journal of Geographical Sciences》 SCIE CSCD 2001年第4期58-68,共10页
The correlations of the d18Omax in the shallow ice core from the Guliya ice cap on the Tibetan Plateau with the global sea surface temperatures (SST) and height at the 500 hPa over the Northern Hemisphere were analyze... The correlations of the d18Omax in the shallow ice core from the Guliya ice cap on the Tibetan Plateau with the global sea surface temperatures (SST) and height at the 500 hPa over the Northern Hemisphere were analyzed. The correlated regions on oceans that have a significant influence on the d18Omax in the Guliya ice core are all located in ocean currents, or convergent regions of currents. They are the eastern Equatorial Pacific, the Northern Pacific Current, the Hot Pool in the eastern Indian Ocean, the Mozambique Current, the Northern Atlantic Current, the Canary Current and the Atlantic Equatorial Current. The d18Omax in the Guliya ice core has negative correlations with the SST located in the lower latitudes, and positive correlations with the SST in the middle latitudes. The correlated areas at the 500 hPa that have a great impact on the d18Omax are located in the subtropical highs over the mid-low-latitude oceans and the long-wave trough area over Balkhash Lake, where there are marked negative correlations between the heights in those areas and the d18Omax. The influencing mechanism is displayed by the diversity of the vapor origins transported to the Guliya region. The strengths of the European ridge and the ridge over Baikal Lake have notable positive correlations with the d18Omax. The two systems indirectly influence the vapor transportation towards the Guliya region by the adjustment of long-wave trough and ridge. 展开更多
关键词 the Tibetan Plateau the Guliya ice core δ18omax SST circulation at 500 hPa correlation
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