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...

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Detalles Bibliográficos
Autores principales: Sun, Y., Ditmar, P., Riva, R.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Berlin Heidelberg 2015
Materias:
Short Note
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

Internet

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

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