Abstract
The Earth’s principal axes and principal moments of inertia, was estimated from the least-squares adjustment of gravitationalharmonic coefficients of second degree of recent global Earth gravity models including EIGEN-1S solution and thedynamical ellipticity derived from the precession constant through VLBI. The estimation was made for the time-independentcomponents (at epoch) of the Earth’s inertial tensor and the time-dependent components of the tensor of inertia, based ongiven information on the secular and periodic variations of harmonic coefficients of second degree.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
