Results 111 to 120 of about 2,359 (214)
Elipsoidal heights determined by GPS is different from orthometric heights used insurveying applications. Therefore, elipsoidal height determined by GPS is transformed to orthometricheight. It can be used several transformation methods to do this transformation.
İNAL, Cevat, YİĞİT, Cemal Özer
openaire +1 more source
The Global navigation satellite systems (GNSS) has imparted positively on civilian positioning & surveying in the horizontal component in Nigeria for the past two decades. The GNSS receivers’ data are longitude, latitude & elevation. However, the vertical distance measurement have not been fully exploited by geodetic and land surveyors.
openaire +2 more sources
Enhanced Vertical Navigation Using Barometric Measurements. [PDF]
Narayanan S, Osechas O.
europepmc +1 more source
A Regional Gravimetric and Hybrid Geoid Model in Northern Greece from Dedicated Gravity Campaigns
The determination of physical heights is of key importance for a wide spectrum of geoscientific applications and, in particular, for engineering projects.
Georgios S. Vergos +7 more
doaj +1 more source
Geopotential models in the Australian region [PDF]
The ability of three high-order geopotential models (OSU81, GPM2 and OSU86E) to recover the gravity anomaly field (delta g) in the Australian region was tested.
Holloway, R. D., Kearsley, A. H. W.
core +1 more source
Vertical datum transformation grids for Mexico. [PDF]
Carrera-Hernández JJ.
europepmc +1 more source
Methodology for the remote transfer of GPS receiver station data through a GSM network. [PDF]
Othman SE, Salama GM, Hamed HFA.
europepmc +1 more source
ICESat-2 Elevation Retrievals in Support of Satellite-Derived Bathymetry for Global Science Applications. [PDF]
Babbel BJ, Parrish CE, Magruder LA.
europepmc +1 more source
Models for extracting vertical crustal movements from leveling data [PDF]
Various adjustment strategies are being used in North America to obtain vertical crustal movements from repeated leveling. The more successful models utilize polynomials or multiquadric analysis to describe elevation change with a velocity surface. Other
Holdahl, S. H.
core +1 more source
The Ohio State 1991 geopotential and sea surface topography harmonic coefficient models [PDF]
The computation is described of a geopotential model to deg 360, a sea surface topography model to deg 10/15, and adjusted Geosat orbits for the first year of the exact repeat mission (ERM).
Pavlis, Nikolaos K. +2 more
core +1 more source

