GRACE��SLR J₂ ��ʱ�����е�С������     

朱广彬  ；李建成  ；  文汉江  ；丁剑 《大地测量与地球动力学》2009,29(4):140-143

????С????????????????С???任????CNES/GRGS??CSR??GFZ???о???????????GRACE???????λ????J2????????н???????????????????????????????SLR???????????J2????????е????????????????????????SLR??????????? J2?????GRACE J2????и???????????仯??????GRACE ???????λ???? J2???л???????161???????????????????????д?????????????S2????????????  相似文献   

根据人卫激光测距、GRACE和地球物理模型求解地球低阶重力场季节变化     

曲伟菁  吴斌  周旭华 《测绘学报》2012,41(6):904-909

本文利用2002年4月至2010年10月的Lageos1和Lageos2两颗激光卫星观测数据、GRACE以及地球物理模型三种独立的方法计算地球低阶重力场系数J 的变化,根据大气压强数据计算 J 时分别按反变气压计（IB）和非反变气压计(NIB)两种假设进行计算。通过分析 J 的季节特性表明,大气在NIB假设下得到的周年振幅比在IB假设下得到的振幅大3倍左右,相位相差47°;大气和陆地水的质量变化对 J 周年变化的贡献占主导地位,海洋的影响最小;大气、海洋和陆地水得到 J 半年振幅和相位值与SLR得到的振幅和相位值吻合较差,尤其是在IB假设下大气得到的结果与SLR结果相差最大; SLR、GRACE和地球物理模型三种独立方法得到的 J 周年项之间吻合相对较好,GRACE得到的周年振幅比SLR得到的周年振幅大50%左右, SLR观测得到的 J 周年振幅介于在NIB和IB两种假设下地球物理模型得到的结果之间;GRACE与SLR得到的 J 半年项的振幅相同,在IB假设下AOW得到的 J 半年振幅和相位与SLR结果差异最大。  相似文献   

Degradation of Geopotential Recovery from Short Repeat-Cycle Orbits: Application to GRACE Monthly Fields     

C. Wagner  D. McAdoo  J. Klokočník  J. Kostelecký 《Journal of Geodesy》2006,80(2):94-103

Throughout 2004 the GRACE (Gravity Recovery And Climate Experiment) orbit contracted slowly to yield a sparse repeat track of 61 revolutions every 4 days on 19 September 2004. As a result, we show from linear perturbation theory that geopotential information previously available to fully resolve a gravity field every month of 120× 120 (degree by order) in spherical harmonics was compressed then into about one-fourth of the necessary observation space. We estimate from this theory that the ideal gravity field resolution in September 2004 was only about 30 × 30. More generally, we show that any repeat-cycle mission for geopotential recovery with full resolution L × L requires the number of orbit-revolutions-to-repeat to be greater than 2L.  相似文献   

地球重力场恢复中的位旋转效应   总被引：6，自引：2，他引：6       下载免费PDF全文

程芦颖  许厚泽 《地球物理学报》2006,49(1):93-98

分析了地球自转引起的位旋转效应公式中采用近似速度的影响. 对一组GFZ的快速科学轨道、一组TUM的约化动力法轨道以及一组GFZ的事后科学轨道，计算了星历提供的速度与只有地球引力场对卫星产生作用时的卫星速度的差值，其中参考重力场模型分别采用EGM96、EIGEN2和EIGEN_CG01C. 通过比较得出：轨道数据与EIGEN2地球重力场模型的自恰性优于EGM96和EIGEN_CG01C地球重力场模型. 速度差各分量的变化具有很明显的周期性且与卫星轨道的运行周期相吻合. 当要求在卫星轨迹处获得1m2/s2精度的扰动位时，也即要求位旋转效应公式中卫星速度的近似精度小于2mm/s时，GFZ的快速科学轨道、TUM的约化动力法轨道只需要剔除那些速度精度不满足要求的卫星轨迹点；当要求在卫星轨迹处获得05m2/s2精度的扰动位时，应当重新估算上述轨道的速度信息，或采用精度更高的GFZ事后科学轨道.  相似文献   

地球外部引力场引起卫星间距离变化的数值模拟研究     

宁津生  罗佳  汪海洪 《武汉大学学报(信息科学版)》2003,28(6):636-641

卫星跟踪卫星(SST)被认为是解决目前地球重力场探测领域中所面临一系列问题的有效方法之一。随着CHAMP、GRACE等SST卫星重力任务的实施，卫星跟踪卫星方法已经进入实用阶段。以GRACE卫星重力计划为参照，利用数值模拟方法研究了由于地球外部引力场导致的卫星间距离变化的规律，得出了相应结论。本研究方法和结论可以为进一步的研究工作，特别是我国未来可能发展的利用SST探测地球重力场的卫星计划提供参考。  相似文献   

Non-isotropic filtering of GRACE temporal gravity for geophysical signal enhancement   总被引：13，自引：0，他引：13  

Shin-Chan Han  C. K. Shum  Christopher Jekeli  Chung-Yen Kuo  Clark Wilson  Ki-Weon Seo 《Geophysical Journal International》2005,163(1):18-25

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卫星重力研究:21世纪大地测量研究的新热点   总被引：18，自引：8，他引：18  

许厚泽 《测绘科学》2001,26(3):1-3

卫星重力发射将大大改善人们对地球重力场的了解 ,最近一些年已经和将要发射的 CHAMP、GRACE及GOCE卫星将把现有静态中长波长部分重力场的精度提高 1- 2个量级 ,并提供长波部分重力场随时间变化的信息。本文对这一大地测量的新进展作了简单叙述  相似文献   

Antenna phase center calibration for precise positioning of LEO satellites   总被引：3，自引：3，他引：3  

Oliver Montenbruck  Miquel Garcia-Fernandez  Yoke Yoon  Steffen Schön  Adrian Jäggi 《GPS Solutions》2009,13(1):23-34

Phase center variations of the receiver and transmitter antenna constitute a remaining uncertainty in the high precision orbit determination (POD) of low Earth orbit (LEO) satellites using GPS measurements. Triggered by the adoption of absolute phase patterns in the IGS processing standards, a calibration of the Sensor Systems S67-1575-14 antenna with GFZ choke ring has been conducted that serves as POD antenna on various geodetic satellites such as CHAMP, GRACE and TerraSAR-X. Nominal phase patterns have been obtained with a robotic measurement system in a field campaign and the results were used to assess the impact of receiver antenna phase patterns on the achievable positioning accuracy. Along with this, phase center distortions in the actual spacecraft environment were characterized based on POD carrier phase residuals for the GRACE and TerraSAR-X missions. It is shown that the combined ground and in-flight calibration can improve the carrier phase modeling accuracy to a level of 4 mm which is close to the pure receiver noise. A 3.5 cm (3D rms) consistency of kinematic and reduced dynamic orbit determination solutions is achieved for TerraSAR-X, which presumably reflects the limitations of presently available GPS ephemeris products. The reduced dynamic solutions themselves match the observations of high grade satellite laser ranging stations to 1.5 cm but are potentially affected by cross-track biases at the cm-level. With respect to the GPS based relative navigation of TerraSAR-X/TanDEM-X formation, the in-flight calibration of the antenna phase patterns is considered essential for an accurate modeling of differential carrier phase measurements and a mm level baseline reconstruction.

Oliver MontenbruckEmail:

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基于GRACE时变重力场反演南极冰盖质量变化   总被引：1，自引：0，他引：1  

李军海  刘焕玲  文汉江  朱广彬  方爱平 《大地测量与地球动力学》2011,31(3):42-46

利用UTCSR发布的GRACE Level-2 RL04版本2003-01—2008-08月的重力场模型估计南极冰盖质量变化。由于GRACE提供的C20项不准确,利用SLR测得的C20项进行替换。对于经度方向上出现的条纹状信号,采用去相关滤波处理。选择去掉其中某一个月的位模型重新反演南极冰盖质量变化,发现相同区域的质量变化率并没有发生很大的变化。联合得到的位模型、滤波技术以及ICE-5G冰后回弹模型观测到的西南极Amundsen地区和南极半岛的冰盖质量消融现象,其等效水高变化分别为-5.28±0.95 cm/a、-1.82±0.77 cm/a;而Ronne冰架以及东部Enderby地区冰盖质量在增加,分别为1.42±0.69 cm/a、1.43±0.72 cm/a。与已有研究结果比较发现：西南极冰盖质量在加速融化,而Ronne冰架以及东部Enderby地区冰盖等效水高变化率没有发生大的变化。  相似文献   

Interpretation of general geophysical patterns in Iran based on GRACE gradient component analysis     

Ramin Kiamehr  Mehdi Eshagh  Lars E. Sjöberg 《Acta Geophysica》2008,56(2):440-454

Only with satellites it is possible to cover the entire Earth densely with gravity field related measurements of uniform quality within a short period of time. However, due to the altitude of the satellite orbits, the signals of individual local masses are strongly damped. Based on the approach of Petrovskaya and Vershkov we determine the gravity gradient tensor directly from the spherical harmonic coefficients of the recent EIGEN-GL04C combined model of the GRACE satellite mission. Satellite gradiometry can be used as a complementary tool to gravity and geoid information in interpreting the general geophysical and geodynamical features of the Earth. Due to the high altitude of the satellite, the effects of the topography and the internal masses of the Earth are strongly damped. However, the gradiometer data, which are nothing else than the second order spatial derivatives of the gravity potential, efficiently counteract signal attenuation at the low and medium frequencies. In this article we review the procedure for estimating the gravity gradient components directly from spherical harmonics coefficients. Then we apply this method as a case study for the interpretation of possible geophysical or geodynamical patterns in Iran. We found strong correlations between the cross-components of the gravity gradient tensor and the components of the deflection of vertical, and we show that this result agrees with theory. Also, strong correlations of the gravity anomaly, geoid model and a digital elevation model were found with the diagonal elements of the gradient tensor.  相似文献