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Preliminary analysis of the applicability of adiabatic modes to inverting synthetic acoustic data in shallow water over a sloping sea floor

机译:绝热模式对倾斜海底浅水中合成声数据反演的适用性的初步分析

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摘要

The May 2001 Geoacoustic Inversion Techniques Workshop provided synthetic transmission loss (TL) data for four cases with range-dependent shallow-water all-liquid environments. In two of these cases ("0" and "1"), the sea floor has constant slope and the geoacoustic model (GAM) is range independent. Cost functions have been computed using a new adiabatic-mode TL algorithm (which uses an exact velocity boundary condition at the sloping sea floor), as one parameter in the GAM is varied. Two frequencies (80 and 220 Hz) were selected. In case 0, the sea-floor slope is 0.0183 and the GAM comprises an inhomogeneous layer over a basement. The sea-floor sound-speed was selected as the variable parameter. The resulting cost minima at 80 and 220 Hz are displaced from the actual sound speed by 2.3 and 3.4 m/s, respectively. In case 1, the sea-floor slope is 0.012 and the GAM comprises one homogenous layer, five inhomogeneous layers, and a basement. The selected parameter was the sound-speed in the homogeneous layer. The corresponding cost minima are displaced by -1.2 and +1.1 m/s. The relative values of these four errors indicate that mode coupling increases with sea-floor slope and that there may be a dependence on frequency at the greater slope.
机译:2001年5月的“地声反演技术研讨会”提供了四种情况下具有范围相关的浅水全液体环境的合成传输损耗(TL)数据。在这两种情况下(“ 0”和“ 1”),海床的坡度恒定,并且地声模型(GAM)与范围无关。由于GAM中的一个参数发生了变化,因此使用新的绝热模式TL算法(在倾斜的海底使用精确的速度边界条件)计算了成本函数。选择了两个频率(80和220 Hz)。在情况0的情况下,海底坡度为0.0183,GAM包含基底上的不均匀层。选择海底声速作为可变参数。在80和220 Hz时产生的最低成本分别与实际声速相差2.3和3.4 m / s。在情况1中,海底坡度为0.012,GAM包括一个均质层,五个非均质层和一个基底。选择的参数是均匀层中的声速。相应的成本最小值偏移了-1.2和+1.1 m / s。这四个误差的相对值表明,模式耦合随着海底坡度的增加而增加,并且在较大坡度处可能对频率有依赖性。

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