2026-06-17T01:26:24Zhttp://doidb.wdc-terra.org/oaip/oai

oai:doidb.wdc-terra.org:77472026-06-10T10:24:03ZDOIDBDOIDB.ISG

false4DOIDB.ISG 10.5880/isg.2016.002 Piñón, Diego Alejandro Diego Alejandro Piñón 0000-0001-8177-6166 National Geographic Institute, Buenos Aires, Argentina Zhang, Kefei Kefei Zhang 0000-0001-9376-1148 The SPACE Research Centre, Royal Melbourne Institute of Technology (RMIT) University, Melbourne, Australia Wu, Suqin Suqin Wu 0000-0002-0994-402X The SPACE Research Centre, Royal Melbourne Institute of Technology (RMIT) University, Melbourne, Australia Cimbaro, Sergio Ruben Sergio Ruben Cimbaro 0000-0003-4788-6171 National Geographic Institute, Buenos Aires, Argentina GFZ Data Services 2016 Geodesy Geoid model ISG Spherical multi-band Fast Fourier Transform Wong-Gore Stokes kernel modification Argentina EARTH SCIENCE > SOLID EARTH > GEODETICS > GEOID CHARACTERISTICS EARTH SCIENCE > SOLID EARTH > GRAVITY/GRAVITATIONAL FIELD > GRAVITY Reguzzoni, Mirko Mirko Reguzzoni 0000-0002-4027-9347 International Service for the Geoid (ISG), Politecnico di Milano, Italy Carrion, Daniela Daniela Carrion 0000-0003-1262-9394 International Service for the Geoid (ISG), Politecnico di Milano, Italy Rossi, Lorenzo Lorenzo Rossi 0000-0001-6050-1972 International Service for the Geoid (ISG), Politecnico di Milano, Italy Piñón, Diego Alejandro National Geographic Institute, Buenos Aires, Argentina ISG Staff International Service for the Geoid (ISG) 2016 Dataset 10.1007/1345_2017_267 10.1111/j.1365-246X.1969.tb00264.x 10.5194/essd-13-1653-2021 http://www.isgeoid.polimi.it/ 1.0 CC BY 4.0 The GEOIDE-Ar16 Argentinian gravimetric geoid model covers the area from 57° S to 20° S in latitude and from 76° W to 52° W in longitude, with a grid resolution of 1' × 1'. It was developed using the remove-compute-restore technique and incorporating the GOCO05S satellite-only global geopotential model up to degree and order 280, together with about 650,000 land and marine gravity measurements. Terrain corrections were calculated for all gravity observations using a combination of the SRTM_v4.1 and SRTM30_Plus_v10 digital elevation models. For the regions that lacked of gravity observations, the DTU13 gravity model was utilised. The residual gravity anomalies were gridded using the tensioned spline algorithm. The resultant gravity anomaly grid was applied in the Stokes' integral using the spherical multi-band FFT approach and the deterministic kernel modification proposed by Wong and Gore. The accuracy of GEOIDE-Ar16 was assessed by comparing it with GPS-levelling derived geoid undulations at 1,904 locations and the EGM2008 model. Results show that the GEOIDE-Ar16 geoid model has an accuracy of less than 10 centimetres.

The geoid model is provided in ISG format 2.0 (ISG Format Specifications), while the file in its original data format is available at the model ISG webpage.
The International Service for the Geoid (ISG) was founded in 1992 (as International Geoid Service - IGeS) and it is now an official service of the International Association of Geodesy (IAG), under the umbrella of the International Gravity Field Service (IGFS). The main activities of ISG consist in collecting, analysing and redistributing local and regional geoid models, as well as organizing international schools on the geoid determination (Reguzzoni et al., 2021).
Gravimetric geoid model: GEOIDEAR16 -76 -52.0162 -57.0007 -20.0167