Using synthetic aperture processing, a chirp sonar generates reflection profiles of the seabed. Synthetic aperture processing is implemented by calculating the vertical change in the positions of acoustic transducers between transmission and using the offsets to time shift the acoustic data so that horizontal reflectors are summed coherently. The calculated changes in the positions of the acoustic transducers between transmission events are based on Doppler velocity log and inertial measurement unit measurements of vehicle motion. Imagery generated from reflection profiles of seabeds with various sediment types are used to quantity the improvement in the spatial resolution and the SNR of reflection profiles as a function of the length of the synthetic aperture. [Work supported by Office of Naval Research.]
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