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- W2002247922 abstract "Measurements made during the GEOSECS (Geochemical Ocean Sections) program in the mixing zone beneath the Two-Degree Discontinuity (TDD) in the western basin of the central Atlantic reveal major breaks in the property-salinity trends at 33°N, 7°S, and 33°S. These fronts divide the western basin sub-TDD mixing zone into two distinct parts. Within each the property-salinity trends are linear and do not vary significantly from station to station. Neither chemical effects nor radioactive decay can be demonstrated. Apparently the residence time of the water is so small that no measurable chemical imprint can develop. On the other hand, the sub-TDD eastern basin waters show 14C aging and respirative and dissolution effects relative to their western basin counterparts. The rates of silica dissolution and CaCO3 dissolution obtained are consistent with independent estimates. The observed 226Ra increase is somewhat smaller than expected suggesting that its input from eastern basin sediments is somewhat lower than the global average." @default.
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- W2002247922 date "1980-06-01" @default.
- W2002247922 modified "2023-09-27" @default.
- W2002247922 title "Hydrography of the central Atlantic—II waters beneath the Two-Degree Discontinuity" @default.
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- W2002247922 doi "https://doi.org/10.1016/0198-0149(80)90052-7" @default.
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