Abstract

Measurements from 57 current meters suspended from anchored buoys in a network between 1.5°N and 1.5°S and from 27.5°W to 35°W in the Atlantic Ocean between February and April 1963 show speeds up to 70 cm/sec within the Equatorial Undercurrent. The bottom of the Undercurrent appears to be no deeper than 150 m; below th is dep th there is a westward-flowing current with speeds up to 25 cm/sec.

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