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卫星跟踪卫星模式中轨道参数需求分析 被引量:14
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作者 郑伟 许厚泽 +3 位作者 钟敏 员美娟 周旭华 彭碧波 《天文学报》 CSCD 北大核心 2010年第1期65-74,共10页
首次基于半解析法利用GRACE(Gravity Recovery and Climate Experiment)双星K波段星间速度误差、GPS接收机轨道误差和加速度计非保守力误差影响累计大地水准面精度的联合模型开展了卫星跟踪卫星模式中轨道参数的需求分析.建议我国将来... 首次基于半解析法利用GRACE(Gravity Recovery and Climate Experiment)双星K波段星间速度误差、GPS接收机轨道误差和加速度计非保守力误差影响累计大地水准面精度的联合模型开展了卫星跟踪卫星模式中轨道参数的需求分析.建议我国将来首颗重力卫星的平均轨道高度设计为400 km和平均星间距离设计为220 km较优.此研究不仅为我国将来卫星重力测量计划中轨道参数的优化选取以及全球重力场精度的有效和快速估计提供了理论基础和计算保证,同时对将来国际GRACE Follow-On地球重力测量计划和GRAIL(Gravity Recovery and Interior Laboratory)月球重力探测计划的发展方向具有一定的指导意义. 展开更多
关键词 天体力学:人造卫星运动 方法:解析 地球:引力场
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Increase in Probability of the Correct Forecast of Tsunami Formation
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作者 V.I. Korochentsev E.V. Lisunov P.P. Sherbakov 《Journal of Environmental Science and Engineering》 2011年第6期716-719,共4页
The presented paper exhibits theory of the "gravitational" waves propagation near the Earth surface and in the ocean. There was determined an expression "gravitational" wave which was registered by the gravimeters... The presented paper exhibits theory of the "gravitational" waves propagation near the Earth surface and in the ocean. There was determined an expression "gravitational" wave which was registered by the gravimeters being placed in several points of the Earth globe. Alteration of gravitational field was accompanied by alteration of the "gravitational" wave which has the velocity differing from the velocity of seismic waves. The theoretical model was proved by many experiments realized under registration of the underwater earthquake core by tens of gravimeters being placed in the Earth globe different points. The "gravitational" waves assist to increase the right forecast probability of the beginning tsunami to 50%. 展开更多
关键词 TSUNAMI EARTHQUAKE gravitational waves tsunami forecast.
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Study on Recovering the Earth's Potential Field Based on GOCE Gradiometry
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作者 SHEN Wenbin LI Jin LI Jiancheng WANG Zhengtao NING Jinsheng CHAO Dingbo 《Geo-Spatial Information Science》 2008年第4期273-278,共6页
Given the second radial derivative Vrr(P) |δs of the Earth's gravitational potential V(P) on the surface δS corresponding to the satellite altitude, by using the fictitious compress recovery method, a fictitio... Given the second radial derivative Vrr(P) |δs of the Earth's gravitational potential V(P) on the surface δS corresponding to the satellite altitude, by using the fictitious compress recovery method, a fictitious regular harmonic field rrVrr(P)^* and a fictitious second radial gradient field V:(P) in the domain outside an inner sphere Ki can be determined, which coincides with the real field V(P) in the domain outside the Earth. Vrr^*(P)could be further expressed as a uniformly convergent expansion series in the domain outside the inner sphere, because rrV(P)^* could be expressed as a uniformly convergent spherical harmonic expansion series due to its regularity and harmony in that domain. In another aspect, the fictitious field V^*(P) defined in the domain outside the inner sphere, which coincides with the real field V(P) in the domain outside the Earth, could be also expressed as a spherical harmonic expansion series. Then, the harmonic coefficients contained in the series expressing V^*(P) can be determined, and consequently the real field V(P) is recovered. Preliminary simulation calculations show that the second radial gradient field Vrr(P) could be recovered based only on the second radial derivative V(P)|δs given on the satellite boundary. Concerning the final recovery of the potential field V(P) based only on the boundary value Vrr (P)|δs, the simulation tests are still in process. 展开更多
关键词 GOCE gradiometry second radial gradients second radial gradient field recovery potential field recovery
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Convergence of Spherical Harmonic Series Expansion of the Earth's Gravitational Potential
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作者 SHEN Wenbin 《Geo-Spatial Information Science》 2009年第1期1-6,共6页
Given a continuous boundary value on the boundary of a "simply closed surface" as that encloses the whole Earth, a regular harmonic fictitious field V*(P) in the domain outside an inner sphere Ki that lies inside... Given a continuous boundary value on the boundary of a "simply closed surface" as that encloses the whole Earth, a regular harmonic fictitious field V*(P) in the domain outside an inner sphere Ki that lies inside the Earth could be determined, and it is proved that V*(P) coincides with the Earth's real field V(P) in the whole domain outside the Earth. Since in the domain outside the inner sphere Ki and the fictitious regular harmonic function V*(P) could be expressed as a uniformly convergent spherical harmonic series, it is concluded that the Earth's potential field could be expressed as a uniformly convergent spherical harmonic expansion series in the whole domain outside the Earth. 展开更多
关键词 potential field fictitious field uniqueness of the solution spherical harmonic series uniform convergence
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