Gravity anomalies in miligals (mGal). === Original Data Source === Geoid model and gravity anomalies for Greenland The Bouguer anomaly grid of Greenland have been derived from a rigorous least-squares collocation downward continuation process of terrain-corrected data, from the same data used to derive the geoid. The Bouguer anomalies are derived for a density of 2.67 g/cm3 over for rock density, and 0.92 g/cm3 for ice thickness. No Bouguer correction have been applied for marine areas, so offshore and data are free-air anomalies. The gravity reference system is GRS80, based on fundamental absolute gravity network. The gravity Faye (free-air) anomaly grid has been restored from the Bouguer anomaly grid by the normal gravity gradient of 0.1119 mGal/m, without terrain corrections, based on the underlying DEM of land and glaciers/ice sheet. Citation: Forsberg R., Jensen T. (2015) New Geoid of Greenland: A Case Study of Terrain and Ice Effects, GOCE and Use of Local Sea Level Data. In: Jin S., Barzaghi R. (eds) IGFS 2014. Int. Association of Geodesy Symposia, vol 144. Springer, https://doi.org/10.1007/1345_2015_50. Citation URL: https://doi.org/10.1007/1345_2015_50