Investigation of the effect of different crustal density models on the gravimetric geoid

Autores
Yilmaz, N.
Año de publicación
2025
Idioma
inglés
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
The geoid is a closed surface representing the Earth's true shape, coinciding with mean sea level. It is used in geodesy to determine the orthometric heights of points. In this study, the e ect of di erent density models on the gravimetric geoid was investigated using the UNB Global Topographical Density Models at 1 arc-degree grid spacing and 30 arc-seconds grid spacing, as well as a constant density value of 2670 kg/m³. The computation of the geoid was based on the ITU_GGC16 global geopotential model. The SRTM model with 1 arcsecond resolution was used as the digital elevation model. Other terrestrial data were obtained from the Colorado region in the western United States.
Facultad de Ciencias Astronómicas y Geofísicas
Materia
Ciencias Astronómicas
Density models
Gravimetric geoid
Model comparison
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by-nc-nd/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/192092

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spelling Investigation of the effect of different crustal density models on the gravimetric geoidYilmaz, N.Ciencias AstronómicasDensity modelsGravimetric geoidModel comparisonThe geoid is a closed surface representing the Earth's true shape, coinciding with mean sea level. It is used in geodesy to determine the orthometric heights of points. In this study, the e ect of di erent density models on the gravimetric geoid was investigated using the UNB Global Topographical Density Models at 1 arc-degree grid spacing and 30 arc-seconds grid spacing, as well as a constant density value of 2670 kg/m³. The computation of the geoid was based on the ITU_GGC16 global geopotential model. The SRTM model with 1 arcsecond resolution was used as the digital elevation model. Other terrestrial data were obtained from the Colorado region in the western United States.Facultad de Ciencias Astronómicas y Geofísicas2025-08info:eu-repo/semantics/conferenceObjectinfo:eu-repo/semantics/publishedVersionResumenhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfhttp://sedici.unlp.edu.ar/handle/10915/192092enginfo:eu-repo/semantics/reference/url/https://sedici.unlp.edu.ar/handle/10915/190232info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-nd/4.0/Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2026-04-23T11:55:40Zoai:sedici.unlp.edu.ar:10915/192092Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292026-04-23 11:55:41.068SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv Investigation of the effect of different crustal density models on the gravimetric geoid
title Investigation of the effect of different crustal density models on the gravimetric geoid
spellingShingle Investigation of the effect of different crustal density models on the gravimetric geoid
Yilmaz, N.
Ciencias Astronómicas
Density models
Gravimetric geoid
Model comparison
title_short Investigation of the effect of different crustal density models on the gravimetric geoid
title_full Investigation of the effect of different crustal density models on the gravimetric geoid
title_fullStr Investigation of the effect of different crustal density models on the gravimetric geoid
title_full_unstemmed Investigation of the effect of different crustal density models on the gravimetric geoid
title_sort Investigation of the effect of different crustal density models on the gravimetric geoid
dc.creator.none.fl_str_mv Yilmaz, N.
author Yilmaz, N.
author_facet Yilmaz, N.
author_role author
dc.subject.none.fl_str_mv Ciencias Astronómicas
Density models
Gravimetric geoid
Model comparison
topic Ciencias Astronómicas
Density models
Gravimetric geoid
Model comparison
dc.description.none.fl_txt_mv The geoid is a closed surface representing the Earth's true shape, coinciding with mean sea level. It is used in geodesy to determine the orthometric heights of points. In this study, the e ect of di erent density models on the gravimetric geoid was investigated using the UNB Global Topographical Density Models at 1 arc-degree grid spacing and 30 arc-seconds grid spacing, as well as a constant density value of 2670 kg/m³. The computation of the geoid was based on the ITU_GGC16 global geopotential model. The SRTM model with 1 arcsecond resolution was used as the digital elevation model. Other terrestrial data were obtained from the Colorado region in the western United States.
Facultad de Ciencias Astronómicas y Geofísicas
description The geoid is a closed surface representing the Earth's true shape, coinciding with mean sea level. It is used in geodesy to determine the orthometric heights of points. In this study, the e ect of di erent density models on the gravimetric geoid was investigated using the UNB Global Topographical Density Models at 1 arc-degree grid spacing and 30 arc-seconds grid spacing, as well as a constant density value of 2670 kg/m³. The computation of the geoid was based on the ITU_GGC16 global geopotential model. The SRTM model with 1 arcsecond resolution was used as the digital elevation model. Other terrestrial data were obtained from the Colorado region in the western United States.
publishDate 2025
dc.date.none.fl_str_mv 2025-08
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info:eu-repo/semantics/publishedVersion
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dc.language.none.fl_str_mv eng
language eng
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Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0)
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rights_invalid_str_mv http://creativecommons.org/licenses/by-nc-nd/4.0/
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