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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. 2 — Monthly RMS of GRACE/GRACE-FO global ocean mass change residuals (in cm of equivalent water height) estimated from the CSR RL06 GSM gravity solutions over the period April 2002 and April 2020 (without SLR $Δ C_{2, 0}$ / $Δ C_{3, 0}$ replacements). The RMS are computed over the open ocean using a 500 km ocean basin kernel and with 300 km Gaussian smoothing. Similar RMS for CSR RL05 GSM solutions are also provided for comparisons