月-日岁差观测

D. Mccarthy, B. Luzum
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引用次数: 1

摘要

本分析中使用的倾角和de观测值来自IERS快速服务和精确分局的组合溶液(McCarthy and Luzum 1991a)。除了对VLBI确定的系数进行校正外,还可以从月球激光测距(LLR)观测中获得额外的估计值(Williams et al. 1991;惠普尔1993)。表? ?将本分析得出的经度和倾角变化估计值与其他作者使用不同观测所得的分析得出的相应项进行比较。Williams(1994)对倾角的理论价值也进行了比较。费率估计数之间存在无法解释的重大差异。分析方法的不同,例如对解中章动系数和相关性的估计程序的不同,可能是造成这些差异的主要原因。在考虑改变国际天文联合会的运动模式时,重要的是要记住,也必须改变岁差常数。引入章动变化而没有相应的进动变化不会改善观测和理论之间的一致性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Observations of Luni-solar precession
The observations of dip and de used in this analysis were taken from the combination solution of the IERS Sub-Bureau for Rapid Service and Precition (McCarthy and Luzum 1991a). Besides correc tions to the coefficients determined from VLBI, additional estimates can be derived from lunar laser ranging (LLR) observations (Williams et al. 1991; Whipple 1993). Table ?? shows a comparison of the estimates of the change in longitude and obliquity derived in this analysis with corresponding terms from analyses by other authors using different observations. The theoretical value of obliquity by Williams (1994) is also included for comparison. There are significant unexplained discrepancies among the rate estimates. Difference in the methods of the analyses such as the procesure for the estimation of the nutation coefficients and correlations within the solutions probably account for the greater part of these discrepancies. In considering the adoption of changes in the IAU model for nuta tion, it is important to recall that changes must also be made in the precession constant. Introduction of changes in nutation without corresponding changes in precession will not improve the agreement between observations and theory.
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