Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/29795
Title: Determination of ocean tide loading displacements in Hong Kong using GPS technique
Authors: Yuan, LG
Ding, XL 
Sun, HP
Zhong, P
Chen, W 
Keywords: GPS
Ocean tide loading
Ocean tide model
Site displacement
Issue Date: 2010
Publisher: Science China Press
Source: Science China. Earth sciences, 2010, v. 53, no. 7, p. 993-1007 How to cite?
Journal: Science China. Earth sciences 
Abstract: Ocean tide loading (OTL) displacements of eight principal constituents at 12 sites in Hong Kong were determined using more than eight years of continuous GPS observations. Parameters of the OTL displacements were estimated using daily GPS solutions obtained with precise point positioning (PPP) technique. The results were compared with predictions from seven latest global ocean tide models. Gravity measurements of OTL in Hong Kong were also used to validate the GPS results. The study shows that the results from both the GPS and gravity measurements agree best with the GOT4.7 and NAO99b models, when the K1 and K2 constituents are excluded. The agreements between the GPS and the model estimates are generally at sub-millimeter level in both the horizontal and vertical directions, except for S2, K2 and K1 constituents that have relatively larger errors. After removing the systematic biases between the GPS and the model estimates, the misfits of M2, S2, N2, O1, P1 and Q1 at all sites are within 0.5 and 1.0 mm in the horizontal and the vertical directions, respectively, whereas K1 and K2 show relatively larger misfits of up to 2.3 mm. Both the GPS and the gravity S2 estimates have large biases with unknown reasons when compared with the modeled values, which needs to be further investigated. The study demonstrates that GPS is capable of estimating the OTL displacements with the same accuracy as the model predictions, especially for coastal areas.
URI: http://hdl.handle.net/10397/29795
ISSN: 1674-7313
EISSN: 1869-1897
DOI: 10.1007/s11430-010-3076-2
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