Acta Geodaetica et Cartographica Sinica ›› 2024, Vol. 53 ›› Issue (2): 252-262.doi: 10.11947/j.AGCS.2024.20230207

• Ocean Satellite Altimetry • Previous Articles     Next Articles

Global marine gravity anomalies recovered from multi-beam laser altimeter data of ICESat-2

LI Zhen1, GUO Jinyun1, SUN Zhongmiao2, JIA Yongjun3, HUANG Lingyong2, SUN Heping4   

  1. 1. College of Geodesy and Geomatics, Shandong University of Science and Technology, Qingdao 266590, China;
    2. State Key Laboratory of Geo-Information Engineering, Xi'an 710054, China;
    3. National Satellite Ocean Application Service, Beijing 100081, China;
    4. Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, Wuhan 430077, China
  • Received:2023-06-08 Revised:2024-01-03 Published:2024-03-08
  • Supported by:
    The National Natural Science Foundation of China (Nos. 42192535; 42274006; 42242015)

Abstract: Satellite altimetry is one of the crucial techniques for the recovery of marine gravity anomalies. The along-track altimeter data is commonly used, while the cross-track data from conventional altimetry missions is not used to recover marine gravity anomalies due to the long time intervals or sparse ground-track spacing, which limits the improvement of the gravity anomaly model. The ICESat-2 laser altimetry mission operates with three pairs of laser beams, each pair separated by 3 km, which provides the possibility of using the cross-track altimeter data. The cross-track data processing method is presented and global marine gravity anomaly models (named IS2Gra_alo and IS2Gra_alo_acr) are recovered from the along-track altimeter data and the combination of along-track and cross-track altimeter data, respectively. The root mean square (RMS) of the difference between IS2Gra_alo_acr and global shipborne gravity is 5.54 mGal, which is 0.16 mGal better than that of IS2Gra_alo. According to the difference between ICESat-2 gravity models and released global gravity anomaly models, the RMS derived by IS2Gra_alo_acr is at least 0.10 mGal better than that of IS2Gra_alo. The above results confirm that the accuracy of the gravity model recovered from along-track data is improved by incorporating cross-track data, and the ICESat-2 altimeter data is reliable for the recovery of global marine gravity anomalies. Additionally, the combination of different cross-track and along-track altimeter data is discussed for the accuracy of the gravity model recovered from ICESat-2. The accuracy of the gravity model is able to be improved by incorporating the appropriate cross-track altimeter data with the along-track altimeter data. This research provides a reference for the recovery of marine gravity anomalies from the future altimeter data of the SWOT altimetry mission and the two-satellite tandem mode altimetry of China.

Key words: ICESat-2, satellite laser altimetry, marine gravity anomaly, deflection of the vertical, sea surface height

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