基于神经网络时空变异性非线性回归的浅水声速估计

E. Zheldak, V. Petukhov, Kiseon Kim
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引用次数: 1

摘要

在没有实际测量的情况下,估计一个地区的繁殖损失的传统方法是使用海洋气候学,这是根据存档数据建立的。通常这种统计模型的分辨率为0.25°-1°。高分辨率的气候学能够更好地反映区域海洋状态,但对于大尺度海洋声学模拟已经足够。随着分辨率的提高,模型的尺寸也随之增大,这使得模型难以应用于小型自主水下系统中,如水下传感器网络节点,由于空间和功率资源有限。为了最小化模型的大小,提出了人工神经网络回归的方法。为验证方法的适用性,选取济州岛附近(东海)浅水区。使用世界海洋数据库2013的数据对神经网络进行训练。利用SAVEX15浅水声实验声速剖面重建数据进行误差估计。虽然预测的均方根误差较大,但声速剖面的垂直梯度重建精度较高,这一点通过传播损失计算得到。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Shallow Water Sound Speed Estimation with Neural Networks-Based Nonlinear Regression of Space-Time Variability
Traditional way to estimate propagation losses in a region with no actual measures is to use oceanographic climatologies, built from archived data. Usually such statistical models have 0.25°-1° resolution. While it is enough for large-scale ocean acoustic simulation, higher-resolution climatology reflects regional ocean state better. With increasing of resolution, size of the models also increases, which makes it difficult to use them in small autonomous underwater systems, such as underwater sensor networks nodes, where space and power resources are limited. To minimize the size of a model the artificial neural network regression is proposed. To check applicability of method, shallow water area near Jeju island (East China Sea) was choosen. Set of neural networks was trained on data from World Ocean Database 2013. To estimate the error of sound speed profile reconstruction data from SAVEX15 shallow water acoustic experiment was used. Although the RMS error of prediction was high, vertical gradients of sound speed profile was reconstructed with good accuracy, which was shown using propagation loss calculations.
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