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Uncertainty in GRACE/GRACE-follow on global ocean mass change estimates due to mis-modeled glacial isostatic adjustment and geocenter motion
Global mean sea level has increased about 3 mm/yr over several decades due to increases in ocean mass and changes in sea water density. Ocean mass, accounting for about two-thirds of the increase, can be directly measured by the Gravity Recovery and Climate Experiment (GRACE) and GRACE Follow-On (GF...
Autores principales: | Kim, Jae-Seung, Seo, Ki-Weon, Chen, Jianli, Wilson, Clark |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2022
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9033860/ https://www.ncbi.nlm.nih.gov/pubmed/35459768 http://dx.doi.org/10.1038/s41598-022-10628-8 |
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