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  2. Drifter (oceanography) - Wikipedia

    en.wikipedia.org/wiki/Drifter_(oceanography)

    Typical sensors acquire air pressure, sea surface temperature, irradiance and salinity. A drifter (not to be confused with a float) is an oceanographic device floating on the surface to investigate ocean currents by tracking location. They can also measure other parameters like sea surface temperature, salinity, barometric pressure, and wave ...

  3. Current meter - Wikipedia

    en.wikipedia.org/wiki/Current_meter

    Using Faraday's law of induction (the third of Maxwell's equations), it is possible to evaluate the variability of the averaged horizontal flow by measuring the induced electric currents. The method has a minor vertical weighting effect due to small conductivity changes at different depths. [3] Tilt Current Meter Operating Principle

  4. Mooring (oceanography) - Wikipedia

    en.wikipedia.org/wiki/Mooring_(oceanography)

    Mooring as deployed in Fram Strait with top buoy, a CTD-sensor, two rotor current meters, acoustic release and train wheels as anchor. A mooring in oceanography is a collection of devices connected to a wire and anchored on the sea floor. It is the Eulerian way of measuring ocean currents, since a mooring is

  5. Weather buoy - Wikipedia

    en.wikipedia.org/wiki/Weather_buoy

    Between 1951 and 1970, a total of 21 NOMAD buoys were built and deployed at sea. [6] Since the 1970s, weather buoy use has superseded the role of weather ships, as they are cheaper to operate and maintain. [7] The earliest reported use of drifting buoys was to study the behavior of ocean currents within the Sargasso Sea in 1972 and 1973. [8]

  6. Rotor current meter - Wikipedia

    en.wikipedia.org/wiki/Rotor_current_meter

    A rotor current meter (RCM) is a mechanical current meter, an oceanographic device deployed within an oceanographic mooring measuring the flow within the world oceans to learn more about ocean currents. Many RCMs have been replaced by instruments measuring the flow by hydroacoustics, the so-called Acoustic Doppler Current Profilers.

  7. Remote sensing (oceanography) - Wikipedia

    en.wikipedia.org/wiki/Remote_sensing_(oceanography)

    To deduce the sea surface height from the satellite height the two-way travel time has to be corrected for dynamical errors, the atmospheric conditions and the local geoid height . The local change of the sea surface height due to dynamical effects like wind and currents can be expressed using the following formula.

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    mail.aol.com

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  9. Ekman current meter - Wikipedia

    en.wikipedia.org/wiki/Ekman_current_meter

    Ekman current meter. The Ekman current meter is a mechanical flowmeter invented by Vagn Walfrid Ekman, a Swedish oceanographer, in 1903.It comprises a propeller with a mechanism to record the number of revolutions, a compass and a recorder with which to record the direction, and a vane that orients the instrument so the propeller faces the current.