Gravity gradient distribution in mainland China from GOCE satellite gravity gradiometry data
At present, gravity field and steady-state ocean circulation explorer (GOCE) gravity data are always used to compute regional gravity anomaly and geoid height. In this study, the latest GOCE gravity field model data (from Oct. 2009 to Jul. 2010) are used to compute the gravity gradient of mainland C...
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| Principais autores: | , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
KeAi Communications Co., Ltd.
2015-01-01
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| Series: | Geodesy and Geodynamics |
| Assuntos: | |
| Acceso en liña: | http://www.sciencedirect.com/science/article/pii/S1674984715000105 |
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