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From Discrete Gravity Survey Data to a High-resolution Gravity Field Representation in the Nordic-Baltic Region
Authors:Silja Märdla  Jonas Ågren  Gabriel Strykowski  Tõnis Oja  Artu Ellmann  René Forsberg
Institution:1. School of Engineering, Tallinn University of Technology, Tallinn, Estoniasilja.mardla@ttu.ee;3. Lantm?teriet, The Swedish Mapping, Cadastral, and Land Registration Authority, G?vle, Sweden;4. National Space Institute, Technical University of Denmark, Lyngby, Denmark;5. Department of Geodesy, Estonian Land Board, Tallinn, Estonia;6. School of Engineering, Tallinn University of Technology, Tallinn, Estonia
Abstract:The deduction of a regularly spaced gravity anomaly grid from scattered survey data is studied, addressing mainly two aspects: reduction of gravity to anomalies and subsequent interpolation by various methods. The problem is illustrated in a heterogeneous study area and contrasting test areas including mountains, low terrains, and a marine area. Provided with realistic error estimates, Least Squares Collocation interpolation of Residual Terrain Model anomalies yields the highest quality gravity grid. In most cases, the Bouguer reduction and other interpolation methods tested are equally viable. However, spline-based interpolation should be avoided in marine areas with trackwise survey data.
Keywords:Bouguer anomaly  gravity database  gridding  interpolation  Nordic Geodetic Commission (NKG)  regional geoid  residual gravity anomaly  Residual Terrain Model (RTM) anomaly
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