Title :
Acoustic vorticity meter for benthic boundary layer flow measurements
Author :
Williams, Albert J. ; Terray, Eugene A. ; Thwaites, Fredrik T. ; Trowbridge, John H.
Author_Institution :
Woods Hole Oceanogr. Instn., MA, USA
Abstract :
An acoustic travel-time flow-meter that had been configured to measure vorticity on scales of 15 and 45 centimeters has now been configured to measure benthic boundary layer vorticity over a scale of 1.5 meters. Closed square paths in each sensor define three orthogonal axes of vorticity. Originally constructed to measure shear in the presence of waves, the 15 cm and 45 cm sensors have an expected accuracy for shear of 10-2 s-1 and 3×10-3 s-1 respectively, The 1.5 m sensor appears to have a noise floor of 2×10-5 s-1. Strong boundary layer shear generates turbulence and turbulent vorticity. Measurements of vorticity are being made with these sensors at several scales in strong tidal flows from 1.2 m to 3.2 m above the bottom. Data are being stored internally and in a pop-up data logger for recovery at the end of the deployment and part way through the deployment, Absolute shear can be determined with the 45 cm sensor through careful zero flow calibration before the deployment. The 1.5 m sensor is part of the deployment tripod and too large to be calibrated in controlled conditions. Consequently, fluctuations in vorticity can be determined with the 1.5 m sensor
Keywords :
acoustic arrays; oceanographic equipment; oceanographic techniques; underwater sound; vortices; accuracy; acoustic travel-time flow-meter; benthic boundary layer flow measurements; calibration; deployment tripod; pop-up data logger; shear generates turbulence; tidal flows; turbulent vorticity; vorticity; Acoustic measurements; Acoustic sensors; Extraterrestrial measurements; Fluid flow measurement; Pollution measurement; Sea measurements; Sea surface; Surface acoustic waves; Vibration measurement; Volume measurement;
Conference_Titel :
OCEANS '94. 'Oceans Engineering for Today's Technology and Tomorrow's Preservation.' Proceedings
Conference_Location :
Brest
Print_ISBN :
0-7803-2056-5
DOI :
10.1109/OCEANS.1994.364205