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Observed changes in the Earth’s dynamic oblateness from GRACE data and geophysical models
A new methodology is proposed to estimate changes in the Earth’s dynamic oblateness ([Formula: see text] or equivalently, [Formula: see text]) on a monthly basis. The algorithm uses monthly Gravity Recovery and Climate Experiment (GRACE) gravity solutions, an ocean bottom pressure model and a glacia...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Springer Berlin Heidelberg
2015
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4750517/ https://www.ncbi.nlm.nih.gov/pubmed/26900263 http://dx.doi.org/10.1007/s00190-015-0852-y |