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Mean Motions in Ptolemy’s Planetary Hypotheses

机译:托勒密行星假说中的平均运动

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In the Planetary Hypotheses, Ptolemy summarizes the planetary models that he discusses in great detail in the Almagest, but he changes the mean motions to account for more prolonged comparison of observations. He gives the mean motions in two different forms: first, in terms of ‘simple, unmixed’ periods and next, in terms of ‘particular, complex’ periods, which are approximations to linear combinations of the simple periods. As a consequence, all of the epoch values for the Moon and the planets are different at era Philip. This is in part a consequence of the changes in the mean motions and in part due to changes in Ptolemy’s time in the anomaly, but not the longitude or latitude, of the Moon, the mean longitude of Saturn and Jupiter, but not Mars, and the anomaly of Venus and Mercury, the former a large change, the latter a small one. The pattern of parameter changes we see suggests that the analyses that yielded the Planetary Hypotheses parameters were not the elegant trio analyses of the Almagest but some sort of serial determinations of the parameters based on sequences of independent observations. Communicated by A. Jones.
机译:在托勒密的《行星假说》中,托勒密总结了他在《天文学家》中详细讨论过的行星模型,但他改变了平均运动以解释更长时间的观测结果。他以两种不同的形式给出平均运动:首先,以“简单,未混合”周期表示,其次,以“特殊,复杂”周期为参考,这些近似于简单周期的线性组合。结果,在菲利普时代,月球和行星的所有纪元值都不相同。这部分是由于平均运动的变化而造成的,部分是由于托勒密在月球异常中的时间发生了变化,而不是月亮的经度或纬度,土星和木星的平均经度,而非火星和金星和水星的异常,前者变化很大,后者很小。我们看到的参数变化模式表明,产生行星假说参数的分析不是Almagest的优雅三重分析,而是基于独立观测序列对参数进行的一系列串行确定。由A. Jones沟通。

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