Experimental earth tidal models in considering nearly diurnal free wobble of the Earth's liquid core  

作　　者：SUNHeping XUJianqiao B.Ducarme 

机构地区：[1]KeyLaboratoryofDynamicGeodesy,InstituteofGeodesyandGeophysics,ChineseAcademyofSciences,Wuhan430077,China [2]ObservatoireRoyaldeBelgique,Av.Circulaire3,B-1180,Brussels,Belgium

出　　处：《Chinese Science Bulletin》2003年第9期935-940,共6页

基　　金：supported jointly by the National Outstanding Youth Science Foundation of China (Grant No.49925411);the Knowledge Innovation Project of the Chinese Academy of Sciences(Grant No.KZCX3-CW-131);the National Natural Science Foundation of China(Grant No.40174022).

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.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.

关 键 词：地球潮汐模型实验 地球流体核心 动态椭圆率 日间自由振动 地球动力学工程 重力 

分 类 号：P312[天文地球—固体地球物理学]