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• W2101035231 startingPage "2574" @default.
• W2101035231 abstract "High 228 Ra/ 226 Ra activity ratios characteristic of waters in the Amazon estuary provide a sensitive indicator of the presence of these waters in the Atlantic Ocean. A conservative mixing model utilizing the 228 Ra/ 226 Ra activity ratio (AR) tied to absolute measurements in the estuary allows us to estimate that 20–34% of the surface water east of the Antilles during June, 5–9% from the same area during December, and 15–20% of the eastern Caribbean surface water during December are derived from the Amazon estuary. Differences in 228 Ra input occur in response to variable stratification of water near the river mouth. During high discharge, intense vertical mixing enriches the water in the estuary in 228 Ra. A large fraction of this water moves to the north and east of the Antilles, where its relatively high 228 Ra/ 226 Ra AR distinguishes it over 1500 km from its source. During low discharge (northern hemisphere fall) a significant fraction of river water passes northwest of the zone of intense mixing into a vertically stratified region where 228 Ra gain is lower. This water is transported by the Guiana Current along the coast of South America and into the Caribbean." @default.
• W2101035231 created "2016-06-24" @default.
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• W2101035231 date "1986-02-15" @default.
• W2101035231 modified "2023-09-25" @default.
• W2101035231 title "Tracing the Amazon component of surface Atlantic water using²²⁸Ra, salinity and silica" @default.
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• W2101035231 doi "https://doi.org/10.1029/jc091ic02p02574" @default.
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