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首页> 外文期刊>Journal of geophysical research. Planets >GLGM-3: A degree-150 lunar gravity model from the historical tracking data of NASA Moon orbiters
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GLGM-3: A degree-150 lunar gravity model from the historical tracking data of NASA Moon orbiters

机译:GLGM-3:学位- 150月球的引力模型美国宇航局月球轨道飞行器的历史跟踪数据

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摘要

In preparation for the radio science experiment of the Lunar Reconnaissance Orbiter (LRO) mission, we analyzed the available radio tracking data of previous NASA lunar orbiters. Our goal was to use these historical observations in combination with the new low-altitude data to be obtained by LRO. We performed Precision Orbit Determination on, trajectory arcs from Lunar Orbiter 1 in 1966 to Lunar Prospector in 1998, using the GEODYN II program developed at NASA Goddard Space Flight Center. We then created a set of normal equations and solved for the coefficients of a spherical harmonics expansion of the lunar gravity potential up to degree and order 150. The GLGM-3 solution obtained with a global Kaula constraint (2.5 x 10 -41-2) shows good agreement with model LP150Q from the Jet Propulsion Laboratory, especially over the nearside. The levels of data fit with both gravity models are very similar (Doppler RMS of -0.2 and -1-2 mm/s in the nominal and extended phases, respectively). Orbit overlaps and uncertainties estimated from the covariance matrix also agree well. GLGM-3 shows better correlation with lunar topography and admittance over the nearside at high degrees of expansion (/ > 100), particularly near the poles. We also present three companion solutions, obtained with the same data set but using alternate inversion strategies that modify the power law constraint and expectation of the individual spherical harmonics coefficients. We give a detailed discussion of the performance of this family of gravity field solutions in terms of observation fit, orbit quality, and geophysical consistency.
机译:在准备收音机的科学实验月球勘测轨道飞行器(LRO)任务,我们分析了可用的无线电跟踪数据前美国宇航局月球轨道飞行器。这些历史观测结合新的低空LRO获得的数据。我们进行精密定轨,从1966年的1号月球轨道轨迹弧线月球探勘者在1998年,使用GEODYN II项目开发的NASA戈达德太空飞行中心。和解决一个球形的系数谐波月球引力的扩张潜在的150度和秩序。解决方案获得全球Kaula约束(2.5 x 10 41-2)显示了良好的协议与模型LP150Q喷气推进实验室,尤其是在左侧的。符合两个重力模型非常相似(多普勒RMS的-0.2和1 - 2毫米/秒的名义和扩展阶段,分别)。重叠和不确定性的估计协方差矩阵也同意。更好地与月球地形和相关性左侧的高程度的导纳扩张(/ > 100),特别是在两极附近。我们还展示了三个同伴的解决方案,获得相同的数据集,但使用交替反转策略修改幂律约束和期望的个人球面谐波系数。给详细讨论的性能这个家庭的重力场的解决方案的观察,轨道质量,地球物理一致性。

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