. Caribbean current survey : spring 1953. Ocean currents. The striking differences in the data from the three ships imply a current system far more flexible than was previously believed to exist. The high surface current speeds found in all three surveys are previously unrecorded features of the circulatory system, a3 is the large eddy inferred from tha USS SAN PABLO observations. This eddy must be of a most transient nature, otherwise it could scarcely have escaped notice so long. Of equal interest are the apparent similarities found during the three surveys, particularly the eddy off Punta M
. Caribbean current survey : spring 1953. Ocean currents. The striking differences in the data from the three ships imply a current system far more flexible than was previously believed to exist. The high surface current speeds found in all three surveys are previously unrecorded features of the circulatory system, a3 is the large eddy inferred from tha USS SAN PABLO observations. This eddy must be of a most transient nature, otherwise it could scarcely have escaped notice so long. Of equal interest are the apparent similarities found during the three surveys, particularly the eddy off Punta Maisi and the persistent eastward drift along the southern coast of c=^, yv. «\^ 41fA if* V£ 33M34 37^^,fl .^4 47/« *fc 30 ^2 *7s. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Keen, D. Jean; Chimiak, Walter; United States. Hydrographic Office. Washington, D. C. : U. S. Navy Hydrographic Office
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Keywords: ., bookauthorunitedstate, bookcentury1900, booksubjectoceancurrents
