Articles | Volume 14, issue 10
https://doi.org/10.5194/essd-14-4589-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/essd-14-4589-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
SDUST2021GRA: global marine gravity anomaly model recovered from Ka-band and Ku-band satellite altimeter data
Chengcheng Zhu
College of Geodesy and Geomatics, Shandong University of Science and Technology, Qingdao, Shandong, China
School of Surveying and Geo-Informatics, Shandong Jianzhu University, Jinan, Shandong, China
College of Geodesy and Geomatics, Shandong University of Science and Technology, Qingdao, Shandong, China
Jiajia Yuan
College of Geodesy and Geomatics, Shandong University of Science and Technology, Qingdao, Shandong, China
School of Geomatics, Anhui University of Science and Technology,
Huainan, Anhui, China
Zhen Li
College of Geodesy and Geomatics, Shandong University of Science and Technology, Qingdao, Shandong, China
Xin Liu
College of Geodesy and Geomatics, Shandong University of Science and Technology, Qingdao, Shandong, China
Jinyao Gao
Key Laboratory of Submarine Geosciences, Second Institute of Oceanography of MNR, Hangzhou, Zhejiang, China
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Short summary
Accurate marine gravity anomalies play an important role in the fields of submarine topography, Earth structure, and submarine exploitation. With the launch of different altimetry satellites, the density of altimeter data can meet the requirements of inversion of high-resolution and high-precision gravity anomaly models. We construct the global marine gravity anomaly model (SDUST2021GRA) from altimeter data (including HY-2A). The accuracy of the model is high, especially in the offshore area.
Accurate marine gravity anomalies play an important role in the fields of submarine topography,...
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