Abstract
It is shown in a geophysical observatory, based on extensive experimental material obtained in the course of joint long-term high-precision gravimetric tidal observations and GPS measurements, that data of the vertical channel of GPS measurements do not currently trace the vertical movement of the Earth’s surface caused by tidal variations. The estimation is obtained for differential GPS measurements and for a separate GPS receiver operating in a dual-frequency mode.
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.
