This document describes in a cookbook-fashion how to obtain geoid height at a given location on the Earth from spherical harmonic coefficients of a gravity model. The document is intended to aid ``the uninitiated oceanographer'' in constructing geoid undulations relative to a given reference ellipsoid, defined by semi-major axis and flattening parameter, to be used with satellite altimetry products
According to the classical Gauss–Listing definition, the geoid is the equipotential surface of the E...
Reference points are needed in any deformation study. Geodesy contributes by measurements and provid...
Abstract:Geoidal undulation is the distance from the surface of an ellipsoid to the surface of a geo...
Geoid determination is the process of calculation of the length of the ellipsoidal normal (geoid und...
Computation of a single geoidal height from gravity acceleration data formally requires that the lat...
Computation of a single geoidal height from gravity acceleration data formally requires that the lat...
The geoid models from GRACE and soon GOCE in combination with sea surface geometry data from satelli...
The geoid models from GRACE and soon GOCE in combination with sea surface geometry data from satelli...
The geoid models from GRACE and soon GOCE in combination with sea surface geometry data from satelli...
The geoid models from GRACE and soon GOCE in combination with sea surface geometry data from satelli...
In geodesy three surfaces, the physical surface of the earth, the geoid and the reference ellipsoid ...
Geoid, the equipotential surface of the earth's gravity field is the surface used as height datum by...
As the surface adopted for geodetic computation is a mathematical surface which is different from th...
International audienceAs the surface adopted for geodetic computation is a mathematical surface whic...
According to the classical Gauss–Listing definition, the geoid is the equipotential surface of the E...
According to the classical Gauss–Listing definition, the geoid is the equipotential surface of the E...
Reference points are needed in any deformation study. Geodesy contributes by measurements and provid...
Abstract:Geoidal undulation is the distance from the surface of an ellipsoid to the surface of a geo...
Geoid determination is the process of calculation of the length of the ellipsoidal normal (geoid und...
Computation of a single geoidal height from gravity acceleration data formally requires that the lat...
Computation of a single geoidal height from gravity acceleration data formally requires that the lat...
The geoid models from GRACE and soon GOCE in combination with sea surface geometry data from satelli...
The geoid models from GRACE and soon GOCE in combination with sea surface geometry data from satelli...
The geoid models from GRACE and soon GOCE in combination with sea surface geometry data from satelli...
The geoid models from GRACE and soon GOCE in combination with sea surface geometry data from satelli...
In geodesy three surfaces, the physical surface of the earth, the geoid and the reference ellipsoid ...
Geoid, the equipotential surface of the earth's gravity field is the surface used as height datum by...
As the surface adopted for geodetic computation is a mathematical surface which is different from th...
International audienceAs the surface adopted for geodetic computation is a mathematical surface whic...
According to the classical Gauss–Listing definition, the geoid is the equipotential surface of the E...
According to the classical Gauss–Listing definition, the geoid is the equipotential surface of the E...
Reference points are needed in any deformation study. Geodesy contributes by measurements and provid...
Abstract:Geoidal undulation is the distance from the surface of an ellipsoid to the surface of a geo...