基于残差补偿的神经网络主被动卫星遥感数据浅海水深反演方法

Shallow Water Depth Inversion Method Based on Residual Compensation for Neural Network Using Active-Passive Satellite Remote Sensing Data

  • 摘要: 随着主被动卫星遥感技术在水深反演领域的广泛应用,其在大范围、快速、高效获取水深信息方面展现出传统水深测量技术难以匹敌的优势,特别是对存在权益争端和边境限制等区域的水深获取具有重要意义。针对现有主被动卫星遥感数据协同水深反演方法在深水区反演精度上仍存在明显不足的问题,提出了一种基于多项式拟合残差分布模型的BP神经网络水深反演方法。该方法首先基于ICESat-2星载激光数据和Sentinel-2遥感数据建立BP神经网络模型,进行初步水深反演;然后基于激光轨迹上光子深度和初始水深反演值,构建多项式残差分布模型,获得反演区域残差分布结果;最后将初步水深反演结果与残差分布结果进行叠加,获得最终水深反演结果。为验证该方法的有效性,选取甘泉岛、东岛和比斯坎湾三个区域进行实验,结果表明,本文方法的RMSE分别为1.14、1.06和0.49 m,均优于现有的水深反演模型,能在不同海底地形条件下取得较好的反演效果。本方法为遥感水深反演技术的发展提供了新的思路和技术支持,有助于提升深水区的反演精度和整体水深反演的可靠性。

     

    Abstract: With the widespread use of active and passive satellite remote sensing technologies for bathymetric inversion, these technologies have been demonstrated their unparalleled advantages over traditional bathymetric measurement techniques in terms of large-scale, rapid, and efficient acquisition of water depth information. This is particularly important for regions with territorial disputes or border restrictions, where obtaining bathymetric data is crucial. This study addresses the issue of limited accuracy in bathymetric inversion in deep-water areas by proposing a BP neural network-based method that uses a polynomial fitting residual distribution model in collaboration with active and passive satellite remote sensing data. First, the method establishes a BP neural network model for preliminary bathymetric inversion using ICESat-2 lidar data and Sentinel-2 remote sensing data. It then creates a residual distribution model, and finally, overlays the preliminary bathymetric inversion results with the residual distribution results to obtain the final water depth inversion. To validate the effectiveness of the proposed method, experiments were conducted in three regions: Ganquan Island, Dong Island, and Biscayne Bay. The results show that the RMSEs of the proposed method are 1.14 m, 1.06 m, and 0.49 m, respectively. These values outperform those of existing bathymetric inversion models and demonstrate good inversion performance under different seabed topography conditions. The method proposed in this study provides new ideas and technical support for developing remote sensing bathymetric inversion technology, helping to improve the inversion accuracy in deep-water areas and the overall reliability of water depth inversion.

     

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