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- W780133908 abstract "For the Iberian Peninsula (-10.5<λ,<5.5, 35<φ<45) a quasigeoid solution has been computed using a global geopotential model, a digital terrain model and point gravity anomalies. The Fast Hartley Transform (FHT) technique has been used in the computations. The effect of topographic masses is taken into account by a residual terrain model (RTM) reduction using a 1000×1000 m DTM in the area. The region was divided into two sub-areas with a common part. Some experiments were performed in order to test the results obtained in each individual sub-area and also in a global calculation for all of the region. Then one solution was calculated at 80692 points in a regular grid covering the region and referred to the GRS80. Results are presented in a contour map." @default.
- W780133908 created "2016-06-24" @default.
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- W780133908 date "1995-01-01" @default.
- W780133908 modified "2023-10-02" @default.
- W780133908 title "The Fast Hartley Transform Applied to the Iberian Geoid Calculation" @default.
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- W780133908 doi "https://doi.org/10.1007/978-3-642-79824-5_46" @default.
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