通过调节张量网络分解重建海洋声速场
Xin Wang1, Kaifei He1,2, Yongjie Qiao3
1College of Oceanography and Space Informatics, China University of Petroleum, Qingdao, 266400, China.
The Journal of the Acoustical Society of America
|March 13, 2026
概括
这项研究引入了一种新的张量模型,用于重建海洋声速场,通过捕捉全球相关性来提高准确性. 完全连接的张量网络-提霍诺夫调节 (FCTN-T) 模型提供比现有方法更快,更精确的结果.
科学领域:
- 海洋学 海洋学 海洋学
- 应用数学 应用数学 应用数学
- 地质物理学 地质物理学
背景情况:
- 对3D海洋声速场 (3D SSF) 的准确重建对于水下声学和海洋学研究至关重要.
- 由于全球相关性分析不足,当前的方法往往难以准确.
研究的目的:
- 开发一种新的,高精度的3DSSF重建方法.
- 通过利用全球相关性和局部流性来解决现有技术的局限性.
主要方法:
- 制定了3D SSF作为第三阶张量.
- 引入了一个低级张量模拟框架:完全连接的张量网络 (FCTN) 模型.
- 将基于因素的提霍诺夫规范化纳入了FCTN框架,创建了FCTN-T模型.
- 开发了一种高效的近接交替最小化 (PAM) 算法,并采用了用于模型优化的加速策略.
主要成果:
- 与最先进的方法相比,FCTN-T模型显示出更高的性能.
- 在重建地面真实3DSSF时取得了更高的准确性.
- 显示了计算速度的显著改进.
结论:
- FCTN-T模型代表了海洋3DSSF重建的重大进步.
- 拟议的方法提供了更准确的海洋声速场的近似值.
- 为研究人员提供更高的准确性和计算效率.
相关概念视频
Deriving the Speed of Sound in a Liquid
1.0K
As with waves on a string, the speed of sound or a mechanical wave in a fluid depends on the fluid's elastic modulus and inertia. The two relevant physical quantities are the bulk modulus and the density of the material. Indeed, it turns out that the relationship between speed and the bulk modulus and density in fluids is the same as that between the speed and the Young's modulus and density in solids.
The speed of sound in fluids can be derived by considering a mechanical wave...
The speed of sound in fluids can be derived by considering a mechanical wave...
1.0K
Uniform Depth Channel Flow: Problem Solving
586
To calculate the flow rate for a trapezoidal channel, first, identify the bottom width, side slope, and flow depth of the channel. The cross-sectional area (A) corresponding to the depth of flow (y), channel bottom width (B), and side slope (θ) is determined by:Next, calculate the wetted perimeter, which includes the bottom width and the sloped side lengths in contact with the water. Using the values of the cross-sectional area and the wetted perimeter, determine the hydraulic radius by...
586
Reconstruction of Signal using Interpolation
816
Signal processing techniques are essential for accurately converting continuous signals to digital formats and vice versa. When a continuous signal is sampled with a period T, the resulting sampled signal exhibits replicas of the original spectrum in the frequency domain, spaced at intervals equal to the sampling frequency. To handle this sampled signal, a zero-order hold method can be applied, which creates a piecewise constant signal by retaining each sample's value until the next...
816
Linear Approximation in Frequency Domain
414
Linear systems are characterized by two main properties: superposition and homogeneity. Superposition allows the response to multiple inputs to be the sum of the responses to each individual input. Homogeneity ensures that scaling an input by a scalar results in the response being scaled by the same scalar.
In contrast, nonlinear systems do not inherently possess these properties. However, for small deviations around an operating point, a nonlinear system can often be approximated as linear....
In contrast, nonlinear systems do not inherently possess these properties. However, for small deviations around an operating point, a nonlinear system can often be approximated as linear....
414
Speed of Sound in Solids and Liquids
4.1K
Most solids and liquids are incompressible—their densities remain constant throughout. In the presence of an external force, the molecules tend to restore to their original positions, which is only possible because the constituents interact. The interactions help the constituents pass on information about external disturbances, like sound waves. Therefore, sound waves travel faster through these media. Compared to solids, the constituents in a liquid are less tightly bound. Thus, sound...
4.1K
Uniform Depth Channel Flow
709
Uniform depth channel flow keeps fluid depth consistent along channels such as irrigation canals. In natural channels, such as rivers, approximate uniform flow is often assumed. This condition occurs when the channel’s bottom slope matches the energy slope, balancing potential energy lost from gravity with head loss due to shear stress. This balance prevents depth changes along the channel length, resulting in a steady, uniform flow.Uniform flow in open channels with a constant cross-section...
709


