Airborne gravimetry has become a vital technique in local gravity field approximation, and upward/downward continuation of gravity data is a key process of airborne gravimetry. In these procedures, the integral domain is divided into two parts, namely the near-zone and the far-zone. The far-zone contributions are approximated by the truncation coefficients and a global geo-potential model, and their values are controlled by several issues. This paper investigates the effects of flight height, the size of near-zone cap, and Remove-Compute-Restore (RCR) technique upon far-zone contributions. Results show that at mountainous area the far-zone contributions can be ignored when EIGEN-6C of 360 degree is removed from the gravity data, together wi...
A comprehensive description is given of a method to compute spherical terrain corrections for gravit...
In February 1998, a regional-scale, airborne gravity survey was carried out over the French Occident...
FALCON airborne gravity gradient data can be converted to vertical gravity via direct integration te...
AbstractAirborne gravimetry has become a vital technique in local gravity field approximation, and u...
To reduce the numerical complexity of inverse solutions to large systems of discretised integral equ...
In situ airborne gravity data at altitudes of 11, 6.3, and 1.7 km over a smooth area of Alabama are ...
This paper studies the contribution of airborne gravity data to improvement of gravimetric geoid mod...
Gravity data gaps in mountainous areas are nowadays often filled in with the data from airborne grav...
To reduce the numerical complexity of inverse solutions to large systems of discretised integral equ...
Spectral gravity forward modelling is a technique that converts a band-limited topography into its i...
Advances in the Global Positioning System (GPS) and strapdown Inertial Navigation System (INS) have ...
Before the computation of short-wavelength and long-wavelength components of the geoid undulations f...
Three methods for evaluating the external accord accuracy of airborne gravity survey line data, name...
Within the modelling of gravity data, a common practice is the upward/downward continuation of the s...
We investigated the Fourier transform-based downward continuation (DWC) of airborne gravity anomalie...
A comprehensive description is given of a method to compute spherical terrain corrections for gravit...
In February 1998, a regional-scale, airborne gravity survey was carried out over the French Occident...
FALCON airborne gravity gradient data can be converted to vertical gravity via direct integration te...
AbstractAirborne gravimetry has become a vital technique in local gravity field approximation, and u...
To reduce the numerical complexity of inverse solutions to large systems of discretised integral equ...
In situ airborne gravity data at altitudes of 11, 6.3, and 1.7 km over a smooth area of Alabama are ...
This paper studies the contribution of airborne gravity data to improvement of gravimetric geoid mod...
Gravity data gaps in mountainous areas are nowadays often filled in with the data from airborne grav...
To reduce the numerical complexity of inverse solutions to large systems of discretised integral equ...
Spectral gravity forward modelling is a technique that converts a band-limited topography into its i...
Advances in the Global Positioning System (GPS) and strapdown Inertial Navigation System (INS) have ...
Before the computation of short-wavelength and long-wavelength components of the geoid undulations f...
Three methods for evaluating the external accord accuracy of airborne gravity survey line data, name...
Within the modelling of gravity data, a common practice is the upward/downward continuation of the s...
We investigated the Fourier transform-based downward continuation (DWC) of airborne gravity anomalie...
A comprehensive description is given of a method to compute spherical terrain corrections for gravit...
In February 1998, a regional-scale, airborne gravity survey was carried out over the French Occident...
FALCON airborne gravity gradient data can be converted to vertical gravity via direct integration te...