The U.S. Coast and Geodetic Survey (NOAA’s predecessor agency) used this style of automatic tide gauge to record water levels until the 1960s.
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The roll of paper turned at a steady rate by the timer and motor on the left side of the machine. A pen set in the holder above the paper traced the rising and falling of tides based on the height of a small float attached to it. The float was attached to the tide machine and housed in a stilling well, a vertical tube that sheltered it from any nearby disturbances in the water.
This Standard Tide Gauge replaced the first version of automatic tide gauges, invented by Joseph Saxton in 1851. Before their advent, tides had to be measured manually by placing a staff marked with units of measurement into the water.
In the mid-1960s, the Standard Tide Gauge was replaced with an analog-to-digital recorder (ADR) tide gauge. These recorded water levels every six minutes, using a punch paper tape system, which could then be fed into a computer for processing. However, tide observers still needed to go out to tide stations and collect the data.
Now, everything is digital. NOAA currently uses an array of sensors at tide monitoring stations that transmit their data every six minutes to satellite and from there to NOAA’s database.
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