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. 2022 Jan 9;43(1):305–345. doi: 10.1007/s10712-021-09685-x

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© The Author(s) 2021

Open AccessThis article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/.

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Fig. 4 — a Annual phasor diagram of barystatic sea level changes observed by satellite altimeter and Argo (Altimeter-Argo) and GRACE CSR RL06 GSM solutions over the period January 2005–December 2015. The five GRACE GSM estimates are based on different treatments of $Δ C_{2, 0}$ (noted as J2 in the legend), ocean basin kernel, and latitude ranges of integration (see Chen et al. 2019 for details); b Annual phasor diagram of barystatic sea level from Altimeter-Argo and GRACE GSM (500 km, GRC J2, ± 64.5) with $Δ C_{0, 0}^{GSM}$ effect considered