Regional analysis of recent global geopotential models: A case study in Turkey
Küçük Resim Yok
Tarih
2017
Yazarlar
Dergi Başlığı
Dergi ISSN
Cilt Başlığı
Yayıncı
International Multidisciplinary Scientific Geoconference
Erişim Hakkı
info:eu-repo/semantics/closedAccess
Özet
Geoid is an equipotential surface of Earth’s gravity field, which partially coincides with the mean sea level and extended inside continents. In the gravimetric geoid determination; global geopotential models (GGMs), digital elevation models and terrestrial gravity observations are combined in a proposed technique (e.g. Remove-Compute-Restore). The external Earth's gravity field is represented by a GGM that consists of the globally and homogeneously distributed terrestrial and satellite gravity measurements. Currently, CHAMP, GRACE, and GOCE satellite missions have been used to determine the gravity field. Satellite-based GGMs that mainly represent the long wavelength components of the gravity field can be evaluated externally by using terrestrial data such as ground gravity, GPS-leveling, etc. Then, the standard deviation of the differences (e.g. NGGM minus NGPS-LEV) is considered as the accuracy of the model. In this study, geoid undulations derived from recently published GGMs are compared with equivalents obtained from GPS-leveling data, and the accuracies of selected GGMs are investigated in the territory of Turkey. Numerical results show that GGMs combining GRACE and GOCE data are more accurate than the others. © SGEM2017. All Rights Reserved.
Açıklama
17th International Multidisciplinary Scientific GeoConference, SGEM 2017 -- 29 June 2017 through 5 July 2017 -- 130787
Anahtar Kelimeler
CHAMP, Global geopotential model, GOCE, GPS-leveling data, GRACE
Kaynak
International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM
WoS Q Değeri
Scopus Q Değeri
N/A
Cilt
17
Sayı
22
