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- W2903069135 abstract "ABSTRACT Radiocarbon ( 14 C) generated by the thermonuclear tests in the late 1950s to early 1960s has been used as a tracer to study atmospheric and oceanic circulations, carbon exchange between different reservoirs, and fossil fuel emissions. Here we report the first measurements of 14 C in atmospheric CO 2 of maritime air collected over the South China Sea (SCS) during July 2014. We also present 14 C of the dissolved inorganic carbon (DIC) in the sea surface water in the same region. Most of the Δ 14 C values of the atmospheric CO 2 vary in the range of 15.6±1.6‰– 22.0±1.6‰, indicating that the central SCS maritime air is well-mixed and consistent with the clean background air in the Northern Hemisphere. The 14 C values of the DIC (DI 14 C) in the surface seawater vary between 28.3±2.5‰ and 40.6±2.7‰, mainly due to the lateral mixing between the SCS and western Pacific. The average surface seawater DI 14 C is 15.4 ± 5.1‰ higher than that of the maritime air 14 CO 2 . The reversal of the sea–air Δ 14 C gradient occurred at ∼2000, marking the start of the upper ocean transferring bomb 14 C back to the atmosphere in the SCS." @default.
- W2903069135 created "2018-12-11" @default.
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- W2903069135 date "2018-12-05" @default.
- W2903069135 modified "2023-10-02" @default.
- W2903069135 title "Radiocarbon in the Maritime Air and Sea Surface Water of the South China Sea" @default.
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- W2903069135 doi "https://doi.org/10.1017/rdc.2018.100" @default.
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