Carbonate Chemistry and the Anthropogenic CO2 in the South China Sea
编号:774 访问权限:仅限参会人 更新:2026-08-31 19:01:53 浏览:0次 特邀报告

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摘要
A little known paper of the same title was published in Acta Oceanologica Sinica in 1995 (Chen and Huang, V14, 47-57). Although it was cited only 28 times compared with my H-index of 86 as of June, 2026, I believe it reported severed new findings:
  • Because of the interference of the submarine topography and the Kuroshio axis, there exists a "front" in the Luzon Strait. East of it, the water mass belongs to the West Philippine Sea, on the west is the mixed water of the South China Sea and the West Philippine Sea.
  • There are only very small differences in biogeochemistry between these two water masses, implying a short deep water residence time of approximately 40 a.
  • The anthropogenic CO2 penetrates to roughly 500 m, slightly shallower than found in the West Philippine Sea. The entire South China Sea contains (0.38±0.1) × 1015 g excess CO2.
Biogeochemical studies have advanced significantly over the past three decades with more accurate and more extensive data partially contributed by the RV Tan Kan Kee. More importantly, now there are enough data to show the effects of global environmental change. Needless to say, time series data such as SEATS (South East Asia Time Series) played a pivotal role. I urge that this station be maintained by all means.
 
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报告人
Chen-Tung Arthur Chen
Outstanding Chair Pr National Sun Yat-sen University

稿件作者
Chen-Tung Arthur Chen National Sun Yat-sen University
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重要日期
  • 会议日期

    01月12日

    2027

    01月15日

    2027

  • 07月21日 2026

    初稿截稿日期

  • 01月15日 2027

    注册截止日期

主办单位
State Key Laboratory of Marine Environmental Science, Xiamen University (MEL)
Department of Earth Sciences, National Natural Science Foundation of China (NSFC)
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