Fusion of Measured and Synthetic
Sound Speed Profiles: A Viable Technique
to Improve the Accuracy of Multibeam
Bathymetry?
Jean-Guy Nistad | Patrick Westfeld
1 Introduction
An important error source in multibeam echo sounder depth measurements in
shallow and highly stratified water column environments is the sound speed er-
ror. The impact of this error in hydrographic data acquisition and processing
is potentially two-fold. First, an incorrectly measured sound speed value at the
echo sounder’s transmit and receive arrays will affect their directivity pattern
steering angles and lead to an erroneous array-relative beam pointing angle.
Second, an incorrectly measured water column sound speed structure will not
account for the true path travelled by the acoustic pulse, because it is affect-
ed by a propagation error in distance and direction. These two impacts lead to
similar yet distinct error signatures, which in both cases propagate to the final
3D point solution referenced in a terrestrial reference frame. While a calibrated
sound speed probe mounted at the antenna arrays should preclude the first error
source, an undersampled water column relative to a changing sound speed struc-
ture in both time and space, inevitably leads to so-called refraction errors. Given
that in-situ knowledge of the water column dynamics is difficult to assess while
surveying and in order to optimize survey time, a common approach is to use
an underway profiling system to increase the number of measured sound speed
profiles. However, excessive profile measurements leading to premature wear of
the profiling system is often the consequence. As such, an optimal sampling pe-
riod that balances cost with survey specifications should always be sought. In
this work, we seek to determine the gain in accuracy achievable by combining
measured with synthetic sound speed profiles to minimize the impact of sound
speed errors in multibeam surveys conducted in the shallow waters of the south-
western Baltic Sea.
Previous work has demonstrated the added value of applying synthetic sound
speed profiles in the absence of measured profiles for multibeam ray-tracing pur-
poses. These synthetic profiles may be derived directly from regional hydrody-
namic models, from spatiotemporal interpolation, or from a combination of the
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