Carbonate Chemistry and the Anthropogenic CO2 in the South China Sea
ID:774
Invited Oral Presentation
2027-01-15 08:30 (China Standard Time)
Session:Session 43 - Biogeochemistry of the South China Sea: The Ten-year expedition of RV Tan Kan Kee
Abstract
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.
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Important Dates
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Jan 30
2026
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2026
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Jan 12–15
2027
XMAS 2027
