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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...

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Detalles Bibliográficos
Autores principales: Kim, Jae-Seung, Seo, Ki-Weon, Chen, Jianli, Wilson, Clark
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
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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