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- W2169122601 abstract "During the 28-month interval from September 1960 through December 1962, drift bottles were released periodically from a stationary platform located 20.4 km offshore from Panama City, Florida. Of the 951 bottles released, 276, or 29 per cent, were recovered. Approximately 67 per cent of the returns have been found along a 350-km section of coastline extending from Cape St. George west to the Florida-Alabama line; 20 per cent of the returns were from the Florida east coast and keys, and 12 per cent were found along the coasts of Alabama, Mississippi, Louisiana, and Texas. Comparison of the drift-bottle data with local wind information indicates that the primary mechanism of surface water transport in the vicinity of the release point is wind-induced currents, which either transport the bottles to local beaches or to regions where permanent or semipermanent currents can displace them to western or southern shores. The results of this study are also compared with other drift-bottle studies conducted in the Gulf of Mexico." @default.
- W2169122601 created "2016-06-24" @default.
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- W2169122601 date "1964-01-15" @default.
- W2169122601 modified "2023-09-23" @default.
- W2169122601 title "Surface circulation of the eastern Gulf of Mexico as determined by drift-bottle studies" @default.
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- W2169122601 doi "https://doi.org/10.1029/jz069i002p00223" @default.
- W2169122601 hasPublicationYear "1964" @default.
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