Current meter

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This article is about a type of oceanographic instrument. For an instrument to measure electrical current, see ammeter.
Propeller-type current meter. The revolutions of the propeller per time intervall are counted electronically.

A current meter is oceanographic device for flow measurement by mechanical (rotor current meter), tilt (Tilt Current Meter), acoustical (ADCP) or electrical means.

Different reference frames[edit]

In physics, one distinguishes different reference frames depending on where the observer is located, this is the basics for the Lagrangian and Eulerian specification of the flow field in fluid dynamics: The observer can be either in the Moving frame (as for a Lagrangian drifter) or at in a resting frame.

Measurement principles[edit]

A buoy deploying a Roberts radio current meter, c. 1960

Mechanical[edit]

Mechanical current meters are mostly based on counting the rotations of a propeller and are thus rotor current meters. A mid-20th-century realization is the Ekman current meter which drops balls into a container to count the number of rotations. The Roberts radio current meter is a device mounted on a moored buoy and transmits its findings via radio to a servicing vessel. Savonius current meters rotate around a vertical axis in order to minimize error introduced by vertical motion.[1]

Acoustic[edit]

A common instrument of this type is the Acoustic Doppler Current Profiler (ADCP) which measures the water current velocities over a depth range using the Doppler effect of sound waves scattered back from particles within the water column. The ADCPs use the traveling time of the sound to determine the position of the moving particles.

Single-point devices use again the Doppler shift, but ignoring the traveling times. Such a single-point Doppler Current Sensor (DCS) has a typical velocity range of 0 to 300 cm/s. The devices are usually equipped with additional optional sensors.

Electromagnetic Induction[edit]

This novel approach is for instance employed in the Florida Strait where electromagnetic induction in submerged telephone cable is used to estimate the through-flow through the gateway[2] and the complete setup can be seen as one huge current meter. The physics behind: Charged particles (the ions in seawater) are moving with the ocean currents in the magnetic field of the Earth which is perpendicular to the movement. 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 electrical currents. The method has a minor vertical weighting effect due to small conductivity changes at different depths.[3]

Tilt Current Meter Operating Principle

Tilt[edit]

Tilt current meters operate under the drag-tilt principle. They consist of a sub-surface buoy that is anchored to the sea floor with a flexible line or tether. The float tilts as a function of its shape, buoyancy and the water velocity. Once the characteristics of a given buoy are known, the velocity can be determined by measuring the angle of the buoy.[4] The buoy contains a data logger that records the orientation (angle from vertical and compass bearing) of the Tilt Current Meter. A Tilt Current Meter is typically deployed on the bottom with an anchor but may be deployed on lobster traps or other convenient anchors of opportunity. [5] A TCM has the advantage over other methods of measuring current in that it is a relatively low cost instrument and the design and operation is simple. However it is not as accurate as an acoustic current meter and unlike an ADCP it only measures current at one depth.

Depth correction[edit]

Current meters are usually deployed within an oceanographic mooring consisting of an anchor weight on the ground, a mooring line with the instrument(s) connected to it and a floating device to keep the mooring line more or less vertical. Like a kite in the wind, the actual shape of the mooring line will not be completely straight, but following a so-called (half-)catenary. Under the influence of water currents (and wind if the top buoy is above the sea surface) the shape of the mooring line can be determined and by this the actual depth of the instruments.[6][7] If the currents are strong (above 0.1 m/s) and the mooring lines are long (more than 1 km), the instrument position may vary up to 50 m.

References[edit]

  1. ^ C. Reid Nichols, Robert G. Williams, Encyclopedia of Marine Science (2008), Infobase Publishing, ISBN 0-8160-5022-8. relevant passages online at Google Books, accessed online 01-26-2012.
  2. ^ Duchez, Aurélie. "Monitoring the MOC at 26.5°N". National Oceanography Centre, Southampton. Retrieved 2012-09-18. 
  3. ^ Meinen, Christopher S. "Florida Current Transport - Project Background". Atlantic Oceanographic & Metereological Laboratory at NOAA. Retrieved 26 September 2012. 
  4. ^ http://www.nefsc.noaa.gov/epd/ocean/MainPage/tilt/shtcm.html
  5. ^ http://www.sciencedaily.com/releases/2010/09/100914102112.htm
  6. ^ Dewey, Richard K. "Mooring Design & Dynamics - A Matlab Package for Designing and Testing Oceanographic Moorings And Towed Bodies". Centre for Earth and Ocean Research, University of Victoria. Retrieved 2012-09-25. 
  7. ^ Dewey, Richard K. (1 December 1999). "Mooring Design & Dynamics—a Matlab® package for designing and analyzing oceanographic moorings". Marine Models 1 (1-4): 103–157. doi:10.1016/S1369-9350(00)00002-X. Retrieved 25 September 2012.