Abstract

The GNSS-acoustic technique is a geodetic method for oceanic areas that combines GNSS positioning of a sea-surface platform and acoustic ranging of seafloor stations. Its positioning accuracy is typically a few and several centimeters for the horizontal and vertical positions, respectively. For further accuracy enhancement, we examined the errors in travel time, the most fundamental data in acoustic ranging. The reference signal used in our observations is a series of sinusoidal waves modulated by binary phase-shift keying with a maximal length sequence whose auto-correlation has a clear main peak at zero lag. However, cross-correlation between the actual returned signal and reference signal is often accompanied by many large sidelobes and looks very different from the synthetic auto-correlation. As a practical measure, we have chosen empirically one peak among several comparable peaks in the cross-correlation, though that is likely to lead to systematic errors in travel time. In this study, we revealed that a variety of cross-correlation waveform primarily depends on the incident angle of acoustic paths and that sidelobes were significantly reduced by substituting phase-only correlation (POC) for conventional cross-correlation. We therefore developed a template-matching technique using POC for the peak detection. POC templates were prepared by stacking actual POCs with certain ranges of the incident angle for each campaign. In the application of this method to actual data, we achieved successful results of our numerous campaign data to date. We consider that POC is advantageous in identifying the main peak uniquely and performing template matching more robustly, because POC enhances short-period components and thus highlights the timing of phase changes further than conventional cross-correlation.

Highlights

  • The GNSS-acoustic (GNSS-A) technique is a geodetic method for ocean areas that combines GNSS positioning of a sea-surface platform and acoustic ranging of seafloor stations (Spiess, 1985)

  • The subsequent wave groups grow as the incident angle decreases, and become even larger than the first main peak group when the incident angle becomes lower than 30°; they continue to grow as the incident angle decreases further

  • We examined the phase-only correlation (POC) of the reference and returned acoustic signals and found that its waveform strongly depends on the incident angle, as it is with the cross-correlation

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Summary

Introduction

The GNSS-acoustic (GNSS-A) technique is a geodetic method for ocean areas that combines GNSS positioning of a sea-surface platform and acoustic ranging of seafloor stations (Spiess, 1985). POC Application to Travel-Time Determination ranging rather than the GNSS positioning of a sea-surface platform. The slant range is calculated from the two-way travel time of the acoustic wave and the sound speed of seawater along the ray path. The both can have significant errors, the scope of this study is the former, that is, the error in travel time. Two-way travel times are determined with a resolution of a few microseconds by calculating the cross-correlation between a reference waveform generated by an onboard transducer and a signal returned from a seafloor transponder. Possible causes for the distortion of the crosscorrelation are the degradation of the signal due to the frequency and phase characteristics of acoustic devices through electro-acoustic transformation, distortion of the returned signal caused by frequency-dependent absorption in seawater, and reflected waves from the surface of a glass sphere of the seafloor transponder or the ship bottom

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