Scientific Reports · 2021 · 17 citations · 34 references
Natural SciencesEarth SciencesOceanographyClimatologyGravityPhysical OceanographyClimate ChangeSea-level ChangeSea-level ReconstructionSea-level VariabilityGlobal Mean Sea LevelGlobal Sea-level ChangeGravity Field RecoveryGravity Recovery And Climate ExperimentMisclosure AnalysisOcean Mass ChangeOcean Mass RedistributionSea-level Budget
Abstract The global sea-level budget is studied using the Gravity Recovery and Climate Experiment (GRACE) solutions, Satellite Altimetry and Argo observations based on the updated budget equation. When the global ocean mass change is estimated with the updated Tongji-Grace2018 solution, the misclosure of the global sea-level budget can be reduced by 0.11–0.22 mm/year compared to four other recent solutions (i.e. CSR RL06, GFZ RL06, JPL RL06 and ITSG-Grace2018) over the period January 2005 to December 2016. When the same missing months as the GRACE solution are deleted from altimetry and Argo data, the misclosure will be reduced by 0.06 mm/year. Once retained the GRACE C 20 term, the linear trends of Tongji-Grace2018 and ITSG-Grace2018 solutions are 2.60 ± 0.16 and 2.54 ± 0.16 mm/year, closer to 2.60 ± 0.14 mm/year from Altimetry–Argo than the three RL06 official solutions. Therefore, the Tongji-Grace2018 solution can reduce the misclosure between altimetry, Argo and GRACE data, regardless of whether the C 20 term is replaced or not, since the low-degree spherical harmonic coefficients of the Tongji-Grace2018 solution can capture more ocean signals, which are confirmed by the statistical results of the time series of global mean ocean mass change derived from five GRACE solutions with the spherical harmonic coefficients truncated to different degrees and orders.
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Global sea-level budget 1993–present
Earth system science data · 2018 · 598 citations · Full text
Donald F. Argus, W. R. Peltier, R. Drummond et al. · Geophysical Journal International · 2014 · 562 citations · Full text