Results 71 to 80 of about 226 (172)
On the Applicability of Molodensky’s Concept of Heights in Planetary Sciences
Geometric heights, defined with respect to a geometric reference surface, are the most commonly used in planetary studies, but the use of physical heights defined with respect to an equipotential surface (typically the geoid) has been also acknowledged ...
Robert Tenzer, Ismael Foroughi
doaj +1 more source
The Accuracy Assessment of the PREM and AK135-F Radial Density Models. [PDF]
Tenzer R, Ji Y, Chen W.
europepmc +1 more source
Lithospheric structural dynamics and geothermal modeling of the Western Arabian Shield. [PDF]
Melouah O +3 more
europepmc +1 more source
The technology for determining a point’s coordinates on the earth’s surface using the global navigation satellite system (GNSS) is becoming the norm along with ground-based methods.
Murat Mustafin, Hiba Moussa
doaj +1 more source
Satellite Gravimetry: A Review of Its Realization. [PDF]
Flechtner F +3 more
europepmc +1 more source
Study on the CHZ-II Gravimeter and Its Calibrations along Forward and Reverse Overlapping Survey Lines. [PDF]
Tu H +7 more
europepmc +1 more source
Conformity of the NASADEM_HGT and ALOS AW3D30 DEM with the Altitude from the Brazilian Geodetic Reference Stations: A Case Study from Brazilian Cerrado. [PDF]
Bettiol GM +4 more
europepmc +1 more source
This study presents the digitization and integration of Kazakhstan’s legacy gravimetric maps at a scale of 1:200,000 into a modern geospatial database using ArcGIS.
Elmira Orynbassarova +5 more
doaj +1 more source
Determining a high-precision national geoid is a fundamental step in modernizing Kazakhstan’s vertical reference system. However, the country’s vast territory, complex topography, and limited coverage of modern terrestrial and airborne gravimetric ...
Daniya Shoganbekova +6 more
doaj +1 more source
Geoid determination using airborne gravity vectors
In traditional airborne gravimetry, the vertical component of the gravity vector is used as an approximation of the measured magnitude of the gravity vector, which enters the determination of the local geoid.
Mehdi Goli +4 more
doaj +1 more source

