SYSU_Topo: A Global Bathymetric Model Derived from SWOT Altimetry and the Gravity-Geological Method
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The Surface Water and Ocean Topography (SWOT) mission provides novel perspectives for ocean observations, including ocean dynamics, marine gravity, and seafloor topography. Based on the gravity anomaly of the grav_SWOT_02 model (released by Scripps Institution of Oceanography), this study uses a high-precision gravity geological method to construct a global seafloor topography model SYSU_Topo with 1 arc-min resolution, focusing on the marine region between 180°W–180°E and 80°S–80°N. To reliably obtain the optimal density contrast for GGM, a sliding window strategy of partition inversion is adopted, and a fusion method with boundary constraint points is developed to effectively eliminate the splicing effect of partition inversion. The model was validated with approximately 11,167,583 independent single-beam bathymetric points and newly added multibeam grid points from GEBCO_2024. The single-beam validation for SYSU_Topo model shows that approximately 87% of the checkpoints have absolute errors within 100 m, while around 89% of the checkpoints exhibit relative errors within 5%. The error distribution of SYSU_Topo model is more concentrated and smaller compared to the topo_27.1 and SDUST2023BCO models. During the multibeam validation, each model demonstrates distinct advantages in specific regions. Notably, the SYSU_Topo model achieves superior performance in the South China Sea, with a std of about 132.07m which is 8%-26% better than other models. Compared to traditional altimeter-derived gravity anomalies, SWOT data exhibits greater potential in filling regions lacking high-precision bathymetry, thereby enhancing seafloor topography inversion accuracy. Even when modelled solely with single-beam data, the SYSU_Topo model achieves reliable precision. This research provides a new benchmark framework for integrating multi-source bathymetric data to construct high-resolution seafloor topography, contributing to the advancement of global ocean mapping efforts.



