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Comparisons of Global Geopotential Models with Terrestrial Gravity Field Data Over Santiago del Estero Region, NW: Argentine

  • L. GalvánEmail author
  • C. Infante
  • E. Lauría
  • R. Ramos
Conference paper
Part of the International Association of Geodesy Symposia book series (IAG SYMPOSIA, volume 136)

Abstract

The recent improvements in satellite tracking data processing, the availability of new surface gravity data sets, and the availability of a new mean sea surface height model from altimetry processing gave rise to the generation of several new global gravity field models. However, to know their potentiality for using in practical situations, we understood that it was necessary their applications in a limited regions. This paper we compare recent geopotential models with gravimetric data over leveling points of Argentinean National Geografhical Institute (ANGI) vertical network in Santiago del Estero region, northwestern Argentine. We have highlighted the most important information, we have established the future expectations to continue with such applications. Results of comparisons are presented.

Keywords

Root Mean Square Altimetry Data Terrestrial Gravity Global Geopotential Model Terrestrial Data 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

Notes

Acknowledgements

The present work has been developed within the framework of the Investigation Project “Evaluation of the elevation global and geopotentials models for the province of Santiago del Estero”, financed by the Council of Investigation of Science and Technical (CICYT) of the National University of Santiago del Estero (UNSE).

To Cristina Pacino by the original idea.

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Copyright information

© Springer-Verlag Berlin Heidelberg 2012

Authors and Affiliations

  1. 1.Faculty of Exact Sciences and TechnologyNational University of Santiago del EsteroSantiago del EsteroArgentine
  2. 2.National Geographical InstituteBuenos AiresArgentine

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