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
.jpg)
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/192092
Ver los metadatos del registro completo
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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. |
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2025 |
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2025-08 |
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http://sedici.unlp.edu.ar/handle/10915/192092 |
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eng |
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eng |
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info:eu-repo/semantics/reference/url/https://sedici.unlp.edu.ar/handle/10915/190232 |
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