By P. Blondel
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Additional info for Bathymetry and Its Applications
Fig. 6. Conductivity-depth sections from 1D inversion using corrected data to account for imperfect AEM instrument calibration. 4 m. The Sow and Pigs reef is shown as a pinnacle at ~ 339900 m (E). The colour scale has units of S/m. 7 S/m. The green section represents sediment and the blue sections represent underlying resistive basement (bedrock). Source: Vrbancich & Fullagar, 2007b. e. by gridding the depth profiles). The upper image was obtained by gridding the known water depths.
J. Acoust. Soc. 90, No. 1, pp. 522-531. de Moustier, C. (1993). F. G. Lourtie (Eds), pp. 329-354. P. & Ishimaru, A. (1986). Application of the composite roughness model to the high frequency bottom backscattering. J. Acoust. Soc. , Vol. 79, No. 5, pp. 1410-1422. P. (1989). Trials and Experimental results of the ECHOES XD Multi-beam Echo sounder. 4, pp. 306-313. G. (1989). A 17,000 year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep -ocean circulation.
Occasional discrete curvilinear, circular or clustered patches of higher backscatter (-32 dB) occur towards the shallower part (Fig. 14). Strong backscatter (-30 to -38 dB) is also observed around the fault. The variation in backscatter observed between these different areas is broadly comparable with results of calibrated acoustical measurements between different known sediment types. Fig. 14. Backscatter strength and bathymetric profiles for three locations and adjacent areas are shown. Stronger backscatter strength from the centres and upper sidewalls are distinctly indicated.
Bathymetry and Its Applications by P. Blondel