Acta Geodaetica et Cartographica Sinica ›› 2026, Vol. 55 ›› Issue (4): 647-657.doi: 10.11947/j.AGCS.2026.20250319

• Coastal and Marine Surveying, Mapping, and Remote Sensing • Previous Articles    

An automated seamount detection method integrating vertical gravity gradient anomaly and seafloor topographic models

Yi GAO1(), Xin LIU1(), Daocheng YU2, Shaoshuai YA1, Shaofeng BIAN3, Heping SUN4, Jinyun GUO1   

  1. 1.College of Geodesy and Geomatics, Shandong University of Science and Technology, Qingdao 266590, China
    2.School of Geomatics, Liaoning Technical University, Fuxin 123000, China
    3.School of Geography and Information Engineering, China University of Geosciences (Wuhan), Wuhan 430074, China
    4.State Key Laboratory of Geodesy and Earth's Dynamics, Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, Wuhan 430077, China
  • Received:2025-08-11 Revised:2026-03-12 Published:2026-05-11
  • Contact: Xin LIU E-mail:2250291272@qq.com;xinliu1969@126.com
  • About author:GAO Yi (2001—), male, postgraduate, majors in satellite altimetry data processing and application. E-mail: 2250291272@qq.com
  • Supported by:
    The National Natural Science Foundation of China(42430101; 42274006; 42192535)

Abstract:

The accurate, global-scale detection of seamounts is of significant importance to the Earth sciences. While traditional shipborne bathymetry methods are costly and have limited coverage, satellite altimetry provides an effective means for identifying seamounts on a global scale. This study proposes an automated seamount detection method that integrates vertical gravity gradient anomalies (VGGAs) and bathymetric models. The method begins by preprocessing the VGGA data with a Gaussian filter to identify local maxima, which are treated as potential seamount centers. Subsequently, closed VGGA contours generated around these centers are subjected to a rigorous screening process based on multiple constraints: area (>50 km2), VGGA amplitude (>12 E), shape fidelity (circular/elliptical fitting errors <10%/15% and a Jaccard index >0.6), and spatial location (excluding continental slopes and their 20 km buffer zones). For regions with complex topography, a marker-controlled watershed algorithm is employed to segment the VGGA signal, after which each subregion is screened independently using the same criteria. Finally, for the candidate regions that pass the screening, the seamount's basal depth is determined by automatically identifying the foot of the slope within the GEBCO_2024 data. This identification is achieved by analyzing the first and second derivatives of bathymetric profiles, enabling an accurate estimation of the seamount's height. Applied to the South China Sea and its surrounding regions, the method identified 278 seamounts taller than 100 m, achieving a 98% spatial match with the SIO 2023 global seamount catalog. Furthermore, our study identified 109potential, previously uncatalogued seamounts. Comparisons with ship-based data demonstrated a root mean square error (RMSE) of 354.4 m in height estimates, validating the method's effectiveness and reliability. This method offers robust technical support for enhancing the global seamount database and advancing related marine research.

Key words: seamount, vertical gravity gradient anomaly, SWOT altimetry satellite, topography seafloor, South China Sea

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