SDUST2020MGCR: a global marine gravity change rate model determined from multi-satellite altimeter data

Investigating the global time-varying gravity field mainly depends on GRACE/GRACE-FO gravity data. However, satellite gravity data exhibit low spatial resolution and signal distortion. Satellite altimetry is an important technique for observing the global ocean and provides many consecutive years of...

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Bibliographic Details
Published in:Earth System Science Data
Main Authors: Zhu, Fengshun, Guo, Jinyun, Zhang, Huiying, Huang, Lingyong, Sun, Heping, Liu, Xin
Format: Text
Language:English
Published: 2024
Subjects:
Online Access:https://doi.org/10.5194/essd-16-2281-2024
https://essd.copernicus.org/articles/16/2281/2024/