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Regional Geoid Models (RGM)

Geodetic Product of EGV: Regional Gravity Field Model
What is a geoid and why is it needed?

The geoid is an equipotential surface of the Earth’s gravity field that closely approximates mean sea level. It represents the hypothetical sea surface that would exist if the oceans were influenced only by Earth’s gravity and rotation, in the absence of external effects such as winds, tides, ocean currents, and variations in atmospheric pressure. As an equipotential surface of the Earth’s gravity field, the geoid has important implications in engineering for the definition of physical heights and for Earth system studies. The most precise technique for determining physical heights above sea level is levelling, but this method is very time consuming and expensive. Today, GNSS/levelling provides a very efficient technology to obtain ellipsoidal heights, from which physical heights can be computed. However, an indispensable requirement for the application of this new methodology is the precise knowledge of the geoid. This underlines the importance of the geoid also for a broad spectrum of surveying and engineering tasks based on the availability of physical heights.

© Reguzzoni et al., 2021 Info Info

Geoid repository: (a) number of available geoid models covering the same area, where blank means missing data; (b) highest spatial resolution of the gridded geoid models available at the International Service for the Geoid (ISG). [Reguzzoni et al., 2021]

Despite the remarkable improvements resulting from the satellite gravity missions CHAMP, GRACE, GRACE Follow-On, and GOCE, the derived global models are limited in terms of spatial resolution due to the dampening of the gravity signal at the satellites altitude. The use of ground, airborne and marine gravity data allows to refine and increase the spatial resolution of the geoid computed from global models. In general, geoid refinement is based on a variety of regional approaches solving a boundary value problem. Therefore, due also to historical reasons, many countries have their own regional (national or local) geoid model.

The International Service for the GEOID

Already in 1992, the International Association of Geodesy (IAG) recognized the need for the establishment of a service to collect and redistribute regional (national, local) geoid models at a worldwide scale, thus making them available to the user community. The International Service for the Geoid (ISG) was born as an IAG Service (formerly known as IGeS, International Geoid Service) within the International Gravity Field Service (IGFS). ISG manages and preserves an openly accessible repository, aiming at storing and redistributing geoid models in standardized data format, providing also ancillary information useful for the geoid application to further analyses. Most models can be freely downloaded, some of them require the author’s permission to be accessible and a few are restricted and cannot be distributed. Since 2020, ISG also provides the assignment of digital object identifiers (DOIs) to the stored geoid models. This is done in collaboration with GFZ Data Services, allowing geoid models being cited in publications.

The main products and tools of the ISG are:

  • Grids of local and regional geoid estimates, collected worldwide (geoid repository)
  • Software for local geoid estimation, terrain gravity effect calculation and global model handling
  • Organization of International schools on geoid determination and thematic courses
  • Publications on Newton’s Bulletin and the former IGeS Bulletin

Data Sources

  • ISG - Geoid Models Repository

    Repository of regional, national and continental geoid models at a worldwide scale at International Service for the Geoid (ISG)

  • Software

    for local geoid estimations

© GGOS (Prepared by: D. Angermann, M. Reguzzoni, T. Gruber, Y. Tanaka)

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PRODUCTS

Global Reference Frames

Celestial Reference Frame (CRF)Terrestrial Reference Frame (TRF)Gravity Reference Frame (GRF)Height Reference Frame (HRF)

Global Earth Gravity Field

Global Gravity Field Models (GGM)Topographic Gravity Field Models (TGFM)Global Gravity Field Quantities (GFQ)

Earth Orientation Parameters

Celestial Pole Offset (CPO)Universal Time (UT1)Length of Day (LOD)Polar Motion (PM)

Satellite Orbits

GNSS Satellite Orbits, Clocks and Biases (GOCB)Earth Observation Satellite Orbits (ESO)

Station Positions and Variations

Station Position Time Series (SPTS)

Atmosphere State

Products of the TroposphereProducts of the ThermosphereProducts of the Ionized Atmosphere

Regional Reference Frames

Regional Terrestrial Reference Frame (RTRF)Regional Gravity Reference Frame (RGRF)Regional Height Reference Frame (RHRF)Vertical Datum Parameter (VDP)

Regional Gravity Field Model

Regional Geoid Model (RGM)Regional Gravity Field Quantities (RGFQ)

Land and Marine Gravity Data

Land Gravity Data (LGD)Marine Gravity Data (MGD)Absolute Gravity Data (AGD)Time Series Gravity Data (TGD)

Sea Surface

Mean Sea Surface (MSS)Sea Level Anomaly (SLA)Sea State (SES)Empirical Ocean Tide Model (EOT)

Sea Level

Global Mean Sea Level / Mean Dynamic Topography (MSL/MDT)Global Sea Level Change / Dynamic Ocean Topography (SLC/DOT)Relative Mean Sea Level (RMSL)Relative Sea Level Change (RSLC)Mean Geostrophic Currents (MGC)

Sea Water Level Records

Sea Water Level Records (SWLR)

Sea Ice

Sea Ice Extension (SIE)Sea Ice Volume (SIV)

Land Geometry

Digital Elevation Model (DEM)Digital Terrain Model (DTM)Plate Kinematic Model (PKM)Earth Surface Deformation (ESD)

Inland Water Level

Mean Regional Water Level (MRWL)Regional Water Level Change (RWLC)

Terrestrial Water Storage

Terrestrial Water Storage Anomaly (TWSA)

Ice Sheets

Ice Mass Change (IMC)Ice Sheet Thickness (IST)

Glaciers

Glacier Mass Change (GMC)Glacier Ice Thickness (GIT)Glacier Flow Velocities (GFV)

IAG as part of the IUGG

  
The International Association of Geodesy (IAG)  is a constituent association of the International Union of Geodesy and Geophysics (IUGG).

IAG Related Organisations

IAG collaborates closely with numerous organizations within geodesy and beyond. See the list for details.

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