Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/29017
Title: The tidal displacement field at Earth's surface determined using global GPS observations
Authors: Yuan, L
Chao, BF
Ding, X 
Zhong, P
Keywords: Body tides
Displacement
Earth's structure
GPS
Lateral heterogeneity
Ocean tidal loading
Issue Date: 2013
Publisher: John Wiley & Sons
Source: Journal of geophysical research. B, Solid earth, 2013, v. 118, no. 5, p. 2618-2632 How to cite?
Journal: Journal of geophysical research. B, Solid earth 
Abstract: We investigate the 3-D tidal displacement field on Earth's surface recorded globally by 456 continuous global positioning system (GPS) stations of IGS spanning 1996-2011, for eight principal diurnal and semidiurnal tidal constituents. In-phase and quadrature amplitudes of the residual tidal displacements, after removal of an a priori body tide model, are estimated using the precise point positioning (PPP) technique on the daily GPS data; the resultant daily estimates are combined to derive final estimates for each tide at each station. The results are compared with the predictions of eight recent global ocean tide models, separately for coastal (307) and inland (149) stations. We show that GPS can provide tidal displacement estimates accurate to the level of 0.12 mm (horizontal) and 0.24 mm (vertical) for the lunar-only constituents (M2, N2, O1, and Q1) and less favorably for solar-related tidal constituents (S2, K2, K1, and P1), although improved by ambiguity resolution. Most recent ocean tide models fit the GPS estimates equally well on the global scale but do not agree well between them in certain coastal areas, especially for the vertical displacements, suggesting the existence of model uncertainties near shallow seas. The tidal residuals for the inland stations after removing both body tides and ocean tidal loading (OTL) furthermore show clear continental-scale spatial coherence, implying deficiencies of the a priori body tide modeling in catching lateral heterogeneity in elastic as well as inelastic properties in the Earth's deep interior. We assert that the GPS tidal displacement estimates now achieve sufficient accuracy to potentially provide constraints on the Earth's structure.
URI: http://hdl.handle.net/10397/29017
ISSN: 2169-9313
EISSN: 2169-9356
DOI: 10.1002/jgrb.50159
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