Seabottom roughness study using a hydrosweep–multibeam system
Seabottom profiling using a multibeam echosounder is a well-known method to acquire a high-resolution and high-density data set for bathymetric mapping of survey area. The use of multibeam echosounder backscatter signals for bottom roughness characterization is a modern technique. Here, the model re...
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Veröffentlicht in: | The Journal of the Acoustical Society of America 1999-02, Vol.105 (2_Supplement), p.1266-1266 |
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creator | Chakraborty, Bishwajit Kodagali, Vijay N. Schenke, Hans W. |
description | Seabottom profiling using a multibeam echosounder is a well-known method to acquire a high-resolution and high-density data set for bathymetric mapping of survey area. The use of multibeam echosounder backscatter signals for bottom roughness characterization is a modern technique. Here, the model results of seabottom backscatter data using a hydrosweep-multibeam system, from some of the geologically well-known areas of Southern Oceans, are presented. Using the capabilities of multibeam systems, angular backscatter strengths are determined employing various corrections. Different bottom backscattering modeling techniques like the composite roughness [Jackson et al., J. Acoust. Soc. Am. 79, 1410–1422 (1986)] and two-layer Helmholtz–Kirchhoff model [Talukdar et al., J. Acoust. Soc. Am. 97, 1545–1558 (1995)] for estimation of bottom roughness is applied. Various seabottom parameters like root-mean-square (rms) relief height, correlation lengths, attenuation coefficients, and layer thickness using the two-layer Helmholtz–Kirchhoff model are calculated. The interface roughness parameters, i.e., slope and intercept values, and volume roughness parameters are computed using the composite roughness theory for the same geological areas. |
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The use of multibeam echosounder backscatter signals for bottom roughness characterization is a modern technique. Here, the model results of seabottom backscatter data using a hydrosweep-multibeam system, from some of the geologically well-known areas of Southern Oceans, are presented. Using the capabilities of multibeam systems, angular backscatter strengths are determined employing various corrections. Different bottom backscattering modeling techniques like the composite roughness [Jackson et al., J. Acoust. Soc. Am. 79, 1410–1422 (1986)] and two-layer Helmholtz–Kirchhoff model [Talukdar et al., J. Acoust. Soc. Am. 97, 1545–1558 (1995)] for estimation of bottom roughness is applied. Various seabottom parameters like root-mean-square (rms) relief height, correlation lengths, attenuation coefficients, and layer thickness using the two-layer Helmholtz–Kirchhoff model are calculated. 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The use of multibeam echosounder backscatter signals for bottom roughness characterization is a modern technique. Here, the model results of seabottom backscatter data using a hydrosweep-multibeam system, from some of the geologically well-known areas of Southern Oceans, are presented. Using the capabilities of multibeam systems, angular backscatter strengths are determined employing various corrections. Different bottom backscattering modeling techniques like the composite roughness [Jackson et al., J. Acoust. Soc. Am. 79, 1410–1422 (1986)] and two-layer Helmholtz–Kirchhoff model [Talukdar et al., J. Acoust. Soc. Am. 97, 1545–1558 (1995)] for estimation of bottom roughness is applied. Various seabottom parameters like root-mean-square (rms) relief height, correlation lengths, attenuation coefficients, and layer thickness using the two-layer Helmholtz–Kirchhoff model are calculated. 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The use of multibeam echosounder backscatter signals for bottom roughness characterization is a modern technique. Here, the model results of seabottom backscatter data using a hydrosweep-multibeam system, from some of the geologically well-known areas of Southern Oceans, are presented. Using the capabilities of multibeam systems, angular backscatter strengths are determined employing various corrections. Different bottom backscattering modeling techniques like the composite roughness [Jackson et al., J. Acoust. Soc. Am. 79, 1410–1422 (1986)] and two-layer Helmholtz–Kirchhoff model [Talukdar et al., J. Acoust. Soc. Am. 97, 1545–1558 (1995)] for estimation of bottom roughness is applied. Various seabottom parameters like root-mean-square (rms) relief height, correlation lengths, attenuation coefficients, and layer thickness using the two-layer Helmholtz–Kirchhoff model are calculated. The interface roughness parameters, i.e., slope and intercept values, and volume roughness parameters are computed using the composite roughness theory for the same geological areas.</abstract><doi>10.1121/1.426055</doi><tpages>1</tpages></addata></record> |
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title | Seabottom roughness study using a hydrosweep–multibeam system |
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