The tidal displacement field at Earth's surface determined using global GPS observations

NCU Institutional Repository > 地球科學學院 > 地球科學學系 > 期刊論文 > Item 987654321/104364

請使用永久網址來引用或連結此文件: https://ir.lib.ncu.edu.tw/handle/987654321/104364

題名:	The tidal displacement field at Earth's surface determined using global GPS observations
作者:	趙丰;Yuan, Linguo;Chao, Benjamin Fong;Ding, Xiaoli;Zhong, Ping
貢獻者:	地球科學學院地球科學學系
關鍵詞:	body tides;Coastal zone;Constituents;Displacement;Diurnal variations;Earth;Earth's structure;Estimates;Geodetics;Geophysics;Global positioning systems;GPS;Heterogeneity;lateral heterogeneity;Mathematical models;ocean tidal loading;Oceans;Stations;Tides
日期:	2013-05-01
上傳時間:	2026-04-23 11:48:49 (UTC+8)
出版者:	Wiley-Blackwell;Washington: Blackwell Publishing Ltd
摘要:	摘要： 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. Key Points3‐D tidal displacements for eight constituents are estimated at 456 IGS stationsThe sub‐millimeter tidal residuals display continental‐scale spatial coherenceThe results can potentially constrain Earth's interior structure 其他題名： J. Geophys. Res. Solid Earth 出版者： Washington: Blackwell Publishing Ltd 出版日期： 2013-05 出處： Journal of geophysical research. Solid earth, 2013-05, Vol.118 (5), p.2618-2632 資源來源： Wiley Online Library - AutoHoldings Journals 版權： 2013. American Geophysical Union. All Rights Reserved. 識別號： ISSN: 2169-9313 識別號： ISSN: 2169-9356 識別號： EISSN: 2169-9356 識別號： DOI: 10.1002/jgrb.50159
顯示於類別:	[地球科學學系] 期刊論文

文件中的檔案:

檔案	描述	大小	格式	瀏覽次數
index.html		0Kb	HTML	14	檢視/開啟

在NCUIR中所有的資料項目都受到原著作權保護.

社群 sharing

資料載入中.....