New solutions for the geoid potential W0 and the Mean Earth Ellipsoid dimensions
Earth Gravitational Models (EGMs) describe the Earth’s gravity field including the geoid, except for its zero-degree harmonic, which is a scaling parameter that needs a known geometric distance for its calibration. Today this scale can be provided by the absolute geoid height as estimated from satel...
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| Hlavní autor: | |
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| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
De Gruyter
2013-12-01
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| Edice: | Journal of Geodetic Science |
| Témata: | |
| On-line přístup: | https://doi.org/10.2478/jogs-2013-0031 |
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