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- W2000769003 abstract "A14C balance for the Eastern Caribbean deep water indicates the average inflow of Atlantic water into the basin to be 2.3 × 105 m3/sec (±30%), or about 2–4 times the values estimated previously. The balance uses a model representation of the deep-water turnover, and is based on14C concentrations at a station in the Venezuelan Basin which average Δ14C= 89‰ below 800 m depth with a total range of only 9‰, as well as on a14C concentration of the Atlantic inflow of Δ14C= −71%. as obtained from measurements outside the Antilles Arch. The turnover time of the basin water below 2500 m depth is 55 years, which corresponds to an average upwelling velocity at this depth of about 35 m/year. With such upwelling, the temperature profile below 1800 m (the depth of the sill determining the inflow of new water) requires a vertical eddy diffusivity of about 5 cm2/sec. The oxygen consumption, and silica and CO2 regeneration, rates below 2500 m depth are obtained as −0.18, + 0.08, and + 0.2 μmole kg−1 yr−1, respectively. The CO2 regeneration has but a negligible effect on the14C balance." @default.
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- W2000769003 date "1976-10-01" @default.
- W2000769003 modified "2023-09-26" @default.
- W2000769003 title "Turnover of Eastern Caribbean deep water from 14C measurements" @default.
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- W2000769003 doi "https://doi.org/10.1016/0012-821x(76)90073-x" @default.
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