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Application of a maximum likelihood processor to acoustic backscatter for the estimation of seafloor roughness parameters

机译:在海底粗糙度参数估计中的应用最大似然处理器对声反向散射的应用

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摘要

Maximum likelihood (ML) estimation is used to extract seafloor roughness parameters from records of acoustic backscatter. The method relies on the Helmholtz–Kirchhoff approximation under the assumption of a power‐law roughness spectrum and on the statistical modeling of bottom reverberation. The result is a globally optimum, highly automated technique that is a useful tool in the context of seafloor classification via remote acoustic sensing. The general geometry of the Sea Beam bathymetric system is incorporated into the design of the ML processor in order to make it applicable to real acoustic data collected by this system. The processor is initially tested on simulated backscatter data and is shown to be very effective in estimating the seafloor parameters of interest. The simulated data are also used to study the effect of data averaging and normalization in the absence of system calibration information. The same estimation procedure is applied to real data collected over two central North Pacific seamounts, Horizon Guyot and Magellan Rise. The Horizon Guyot results are very close to estimates obtained through a curve‐fitting procedure presented by de Moustier and Alexandrou [J. Acoust. Soc. Am. 90, 522–531 (1991)]. In the case of Magellan Rise, discrepancies are observed between the results of ML estimation and curve fitting.
机译:最大可能性(ML)估计用于从声反向散射记录中提取海底粗糙度参数。该方法依赖于掌权粗糙度频谱的假设下的Helmholtz-Kirchhoff近似值,并依靠底部混响的统计建模。结果是全球最佳,高度自动化的技术,是通过远程声学传感的海底分类的上下文中的一个有用工具。海边梁宽度系统的一般几何形状被纳入M1处理器的设计中,以使其适用于该系统收集的实际声学数据。处理器最初在模拟的反向散射数据上进行测试,并且被证明在估计感兴趣的海底参数方面非常有效。模拟数据还用于研究数据平均和归一化在没有系统校准信息的情况下的影响。相同的估计程序适用于由两艘中央北太平洋海山,地平线Guyot和Magellan崛起收集的真实数据。 Horizo​​ n Guyot结果非常接近通过De Moustier和Alexandrou提出的曲线拟合程序获得的估计[J. acoust。 SOC。是。 90,522-531(1991)]。在麦哲伦崛起的情况下,在M1估计和曲线拟合的结果之间观察到差异。

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