AI Article Synopsis

  • An innovative in-situ laser Doppler current probe (LDCP) is introduced for measuring micro-scale subsurface current speed and analyzing micron particle characteristics simultaneously.
  • The LDCP uses dual wavelength lasers, allowing it to effectively capture the velocity components of ocean currents while also determining the size distribution of suspended particles in detail.
  • Field tests in the Yellow Sea confirmed that the LDCP is a valuable tool for ongoing studies of plankton communities and ocean dynamics, aiding in understanding carbon cycle processes.

Article Abstract

An in-situ laser Doppler current probe (LDCP) for the simultaneous measurements of the micro-scale subsurface current speed and the characterizations of micron particles is dedicated in this paper. The LDCP performs as an extension sensor for the state-of-the-art laser Doppler anemometry (LDA). The all-fiber LDCP utilized a compact dual wavelength (491 nm and 532 nm) diode pumped solid state laser as the light source to achieve the simultaneous measurements of the two components of the current speed. Besides its ability for the measurements of the current speed, the LDCP is also capable of obtaining the equivalent spherical size distribution of the suspended particles within small size range. The micro-scale measurement volume formed by two intersecting coherent laser beams makes it possible to accurately estimate the size distribution of the micron suspended particles with high temporal and spatial resolution. With its deployment during the field campaign at Yellow Sea, the LDCP has been experimentally demonstrated as an effective instrument to capture the micro-scale subsurface ocean current speed. The algorithm for retrieving the size distribution of the small suspended particles (2∼7.5µm) has been developed and validated. The combined LDCP system could be applied to the continuous long-term observations of plankton community structure, ocean water optical parameter over a wide range, and useful to elucidate the processes and interactions of the carbon cycles in the upper ocean.

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Source
http://dx.doi.org/10.1364/OE.483575DOI Listing

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