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The log was a simple float the Challenger scientists
used to measure surface current. From an anchored boat, sailors threw the
log attached to a rope into the water. Scientists noted the direction the
log was moved by the current. After a period of time passed, they measured
the length of rope pulled overboard by the float and divided this distance
by the time, to get the speed of the surface current. The
current drag measured currents below the surface. The weighted drag hung
below a surface float so it could drift along in deeper currents. Scientists
calculated the velocity of the drag's surface float, and taking into account
the surface current measured with a log, they calculated the velocity
of the deeper current.
Modern current meters have various designs. Basically they
either move with the current as drifters, or are stationary and hold one
position as the water moves past.
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