SDUST2023VGGA: a global ocean vertical gradient of gravity anomaly model determined from multidirectional data from mean sea surface
Ruichen Zhou,Jinyun Guo,Shaoshuai Ya,Heping Sun,and Xin Liu
Ruichen Zhou
College of Geodesy and Geomatics, Shandong University of Science and Technology, Qingdao 266590, China
State Key Laboratory of Precision Geodesy, Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, Wuhan 430077, China
College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China
College of Geodesy and Geomatics, Shandong University of Science and Technology, Qingdao 266590, China
Shaoshuai Ya
College of Geodesy and Geomatics, Shandong University of Science and Technology, Qingdao 266590, China
Heping Sun
State Key Laboratory of Precision Geodesy, Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, Wuhan 430077, China
Xin Liu
College of Geodesy and Geomatics, Shandong University of Science and Technology, Qingdao 266590, China
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Total article views: 3,693 (including HTML, PDF, and XML)
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Total article views: 2,617 (including HTML, PDF, and XML)
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Total article views: 1,076 (including HTML, PDF, and XML)
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SDUST2023VGGA is a high-resolution (1' × 1') model developed to map the ocean's vertical gradient of gravity anomaly. By using multidirectional mean sea surface data, it reduces the impact of ocean dynamics and provides detailed global gravity anomaly change rates. This model provides critical insights into seafloor structures and ocean mass distribution, contributing to research in marine geophysics and oceanography. The dataset is freely available on Zenodo.
SDUST2023VGGA is a high-resolution (1' × 1') model developed to map the ocean's vertical...