R Tenzer, K Hamayun, P Vajda - Journal of Geophysical …, 2009 - Wiley Online Library
We use the CRUST 2.0 crustal model and the EGM08 geopotential model to compile global maps of the gravity disturbances corrected for the gravitational effects (attractions) of the …
This article reviews a spectral forward gravity field modelling method that was initially designed for topographic/isostatic mass reduction of gravity data. The method transforms 3D …
YM Wang, J Saleh, X Li, DR Roman - Journal of Geodesy, 2012 - Springer
A new gravimetric geoid model, USGG2009 (see Abbreviations), has been developed for the United States and its territories including the Conterminous US (CONUS), Alaska …
This paper represents a milestone in the UNB effort to formulate an accurate and self- consistent theory for regional geoid determination. To get the geoid to a sub-centimetre …
J Huang, M Véronneau - Journal of geodesy, 2013 - Springer
A new gravimetric geoid model, Canadian Gravimetric Geoid 2010 (CGG2010), has been developed to upgrade the previous geoid model CGG2005. CGG2010 represents the …
We analyse spatial and spectral characteristics of various refined gravity data used for modelling and gravimetric interpretation of the crust–mantle interface and the mantle …
A Ellmann, P Vaníček - Journal of Geodynamics, 2007 - Elsevier
Over the past two decades the so-called Stokes–Helmert method has been used for regional geoid determination at the University of New Brunswick (UNB). The present contribution …
In geophysical studies investigating the lithosphere structure, the gravitational field generated by the ocean density contrast (ie, bathymetry-generated gravitational field) …
In geophysical studies investigating the lithosphere structure, topographic, bathymetric, and density contrasts stripping corrections are applied to gravity data. The ocean density contrast …