Applied Research Laboratories, University of Texas at Austin, 10000 Burnet Road, Austin, Texas 78758, USA.
J Acoust Soc Am. 2012 Apr;131(4):2587-98. doi: 10.1121/1.3687446.
Three-dimensional propagation effects of low frequency sound from 100 to 400 Hz caused by seafloor topography and range-dependent bottom structure over a 20 km range along the New Jersey shelf are investigated using a hybrid modeling approach. Normal modes are used in the vertical dimension, and a parabolic-equation approximate model is applied to solve the horizontal refraction equation. Examination of modal amplitudes demonstrates the effect of environmental range dependence on modes trapped in the water column, modes interacting with the bottom, and modes trapped in the bottom. Using normal mode ray tracing, topographic features responsible for three-dimensional effects of horizontal refraction and focusing are identified. These effects are observed in the measurements from the Shallow Water 2006 experiment. Specifically, signals from a pair of fixed sources recorded on a horizontal line array sitting on the seafloor show an intensification caused by horizontal focusing due to the seabed topography of 4 dB along the array.
利用混合建模方法研究了新泽西大陆架 20 公里范围内海底地形和随距离变化的海底结构对 100 至 400 Hz 低频声音的三维传播效应。垂直方向采用模态,水平折射方程采用抛物线近似模型求解。模态幅度的研究表明环境随距离变化对被困在水柱中的模态、与海底相互作用的模态和被困在海底中的模态的影响。利用模态射线追踪,确定了导致水平折射和聚焦三维效应的地形特征。这些效应在 2006 年浅海实验的测量中观察到。具体来说,在海底水平线列阵上记录的一对固定声源的信号由于海底地形,在阵列上产生了 4 dB 的水平聚焦增强。