Reference : Vertical crustal motion observed in the BIFROST project |
Scientific journals : Article | |||
Physical, chemical, mathematical & earth Sciences : Earth sciences & physical geography Physical, chemical, mathematical & earth Sciences : Physics | |||
http://hdl.handle.net/10993/832 | |||
Vertical crustal motion observed in the BIFROST project | |
English | |
Scherneck, Hans-Georg [Chalmers University of Technology, Onsala Space Observatory, Sweden] | |
Johansson, Jan M. [Chalmers University of Technology, Onsala Space Observatory, Sweden] | |
Koivula, Hannu [Finnish Geodetic Institute, Masala, Finland] | |
van Dam, Tonie ![]() | |
Davis, James L. [Harvard-Smithsonian Center for Astrophysics, Cambridge, USA] | |
2003 | |
Journal of Geodynamics | |
Elsevier Science Ltd. | |
35 | |
4-5 | |
425-441 | |
Yes (verified by ORBilu) | |
0264-3707 | |
[en] GIA ; GPS ; sea-level ; tectonics | |
[en] This paper reports from investigations on the robustness of estimated rates of intraplate motion from the continuous GPS project BIFROST (Baseline Inferences from Fennoscandian Rebound Observations, Sealevel and Tectonics). We study loading effects due to ocean, atmosphere and hydrology and their impact on estimated rate parameters. We regularly find the admittance of a modelled perturbation at less than fifty percent of the full effect. We think that the finding relates to a difficult noise situation at all periods, and that a satisfying model for the dominating noise source has not been found yet. An additional reason for low admittance is found in the mapping process of the no-fiducial network solution into a conventional reference frame. | |
Researchers | |
http://hdl.handle.net/10993/832 | |
10.1016/S0264-3707(03)00005-X |
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