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Conversion of time-varying Stokes coefficients into mass anomalies at the Earth’s surface considering the Earth’s oblateness
Time-varying Stokes coefficients estimated from GRACE satellite data are routinely converted into mass anomalies at the Earth’s surface with the expression proposed for that purpose by Wahr et al. (J Geophys Res 103(B12):30,205–30,229, 1998). However, the results obtained with it represent mass tran...
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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Springer Berlin Heidelberg
2018
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Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6405182/ https://www.ncbi.nlm.nih.gov/pubmed/30930553 http://dx.doi.org/10.1007/s00190-018-1128-0 |