Accuracy of a Pulse-Coherent Acoustic Doppler Profiler in a Wave-Dominated Flow
Jessica R. Lacy, Christopher R. Sherwood
Abstract
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Jessica R. Lacy, Christopher R. Sherwood
Abstract
Open-access reader
The accuracy of velocities measured by a pulse-coherent acoustic Doppler profiler (PCADP) in the bottom boundary layer of a wave-dominated inner-shelf environment is evaluated.The downward-looking PCADP measured velocities in eight 10-cm cells at 1 Hz.Velocities measured by the PCADP are compared to those measured by an acoustic Doppler velocimeter for wave orbital velocities up to 95 cm s Ϫ1 and currents up to 40 cm s Ϫ1 .An algorithm for correcting ambiguity errors using the resolution velocities was developed.Instrument bias, measured as the average error in burst mean speed, is Ϫ0.4 cm s Ϫ1 (standard deviation ϭ 0.8).The accuracy (root-mean-square error) of instantaneous velocities has a mean of 8.6 cm s Ϫ1 (standard deviation ϭ 6.5) for eastward velocities (the predominant direction of waves), 6.5 cm s Ϫ1 (standard deviation ϭ 4.4) for northward velocities, and 2.4 cm s Ϫ1 (standard deviation ϭ 1.6) for vertical velocities.Both burst mean and root-meansquare errors are greater for bursts with u b Ն 50 cm s Ϫ1 .Profiles of burst mean speeds from the bottom five cells were fit to logarithmic curves: 92% of bursts with mean speed Ն 5 cm s Ϫ1 have a correlation coefficient R 2 Ͼ 0.96.In cells close to the transducer, instantaneous velocities are noisy, burst mean velocities are biased low, and bottom orbital velocities are biased high.With adequate blanking distances for both the profile and resolution velocities, the PCADP provides sufficient accuracy to measure velocities in the bottom boundary layer under moderately energetic inner-shelf conditions.
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The accuracy of velocities measured by a pulse-coherent acoustic Doppler profiler (PCADP) in the bottom boundary layer of a wave-dominated inner-shelf environment is evaluated.The downward-looking PCADP measured velocities in eight 10-cm cells at 1 Hz.Velocities measured by the PCADP are compared to those measured by an acoustic Doppler velocimeter for wave orbital velocities up to 95 cm s Ϫ1 and currents up to 40 cm s Ϫ1 .An algorithm for correcting ambiguity errors using the resolution velocities was developed.Instrument bias, measured as the average error in burst mean speed, is Ϫ0.4 cm s Ϫ1 (standard deviation ϭ 0.8).The accuracy (root-mean-square error) of instantaneous velocities has a mean of 8.6 cm s Ϫ1 (standard deviation ϭ 6.5) for eastward velocities (the predominant direction of waves), 6.5 cm s Ϫ1 (standard deviation ϭ 4.4) for northward velocities, and 2.4 cm s Ϫ1 (standard deviation ϭ 1.6) for vertical velocities.Both burst mean and root-meansquare errors are greater for bursts with u b Ն 50 cm s Ϫ1 .Profiles of burst mean speeds from the bottom five cells were fit to logarithmic curves: 92% of bursts with mean speed Ն 5 cm s Ϫ1 have a correlation coefficient R 2 Ͼ 0.96.In cells close to the transducer, instantaneous velocities are noisy, burst mean velocities are biased low, and bottom orbital velocities are biased high.With adequate blanking distances for both the profile and resolution velocities, the PCADP provides sufficient accuracy to measure velocities in the bottom boundary layer under moderately energetic inner-shelf conditions.
Key concepts: Standard deviation, Root mean square, Physics, Doppler effect, Geology, Geodesy, Mean squared error, Mean flow