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- W122221581 abstract "High-degree (Nmax=360) gravitational models require surface gravity data to resolve the fine structure of the field. Given a global gravity anomaly data set, one can extract this information using either quadrature formulae (orthogonality relations) or by solving a system of observation equations. Under certain conditions such a system yields a normal matrix of block-diagonal structure. To determine accurately the lower part of the spectrum requires the least-squares combination of the surface gravity information with a satellite-only gravity model. Depending on the technique employed to develop the surface gravity solution, the estimation of a combined model can be performed in different ways." @default.
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- W122221581 date "1996-01-01" @default.
- W122221581 modified "2023-09-23" @default.
- W122221581 title "Alternative Estimation Techniques for Global High-Degree Gravity Modeling" @default.
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- W122221581 doi "https://doi.org/10.1007/978-3-642-61140-7_11" @default.
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