Experimental earth tidal models in considering nearly diurnal free wobble of the Earth's liquid core
文献类型:期刊论文
作者 | Sun, H. P. ; Xu, J. Q. ; Ducarme, B. |
刊名 | Chinese Science Bulletin
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出版日期 | 2003 |
期号 | 9页码:935-940 |
中文摘要 | Based on the 28 series of the high precision and high minute sampling tidal gravity observations at 20 stations in Global Geodynamics Project (GGP) network, the resonant parameters of the Earth's nearly diurnal free wobble (including the eigenperiods, resonant strengths and quality factots) are precisely determined. The discrepancy of the eigenperiod between observed and theoretical values is studied, the important conclusion that the real dynamic ellipticity of the liquid core is about 5% larger than the one under the static equilibrium assumption is approved by using our gravity technique. The experimental Earth's tidal gravity models with considering the nearly diurnal free wobble of the Earth's liquid core are constructed in this study. The numerical results show that the difference among three experimental models is less than 0.1%, and the largest discrepancy compared to those widely used nowdays given by Dehant (1999) and Mathews (2001) is only about 0.4%. It can provide with the most recent real experimental tidal gravity models for the global study of the Earth's tides, geodesy and space techniques and so on. |
原文出处 | |
公开日期 | 2012-04-11 |
源URL | [http://ir.whigg.ac.cn/handle/342008/3267] ![]() |
专题 | 测量与地球物理研究所_其他_期刊论文 |
推荐引用方式 GB/T 7714 | Sun, H. P.,Xu, J. Q.,Ducarme, B.. Experimental earth tidal models in considering nearly diurnal free wobble of the Earth's liquid core[J]. Chinese Science Bulletin,2003(9):935-940. |
APA | Sun, H. P.,Xu, J. Q.,&Ducarme, B..(2003).Experimental earth tidal models in considering nearly diurnal free wobble of the Earth's liquid core.Chinese Science Bulletin(9),935-940. |
MLA | Sun, H. P.,et al."Experimental earth tidal models in considering nearly diurnal free wobble of the Earth's liquid core".Chinese Science Bulletin .9(2003):935-940. |
入库方式: OAI收割
来源:测量与地球物理研究所
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