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行星共振对月球偏心率的激发

Excitation of lunar eccentricity by planetary resonances.

作者信息

Cuk Matija

机构信息

Department of Physics and Astronomy, University of British Columbia, 6224 Agricultural Road, Vancouver, BC V6T 1Z1, Canada.

出版信息

Science. 2007 Oct 12;318(5848):244. doi: 10.1126/science.1146984.

DOI:10.1126/science.1146984
PMID:17932291
Abstract

The origin of the Moon's nonnegligible orbital eccentricity of 0.053 has no theoretical explanation. Lunar laser ranging indicates that tides on Earth are currently increasing the Moon's eccentricity. However, ocean tides were likely much weaker during the first billion years, allowing lunar tides to damp any primordial lunar eccentricity very early on. During the tidally driven expansion of its orbit, the Moon must have been affected by two substantial resonances related to Jupiter and Venus, passage through which may have generated today's lunar eccentricity.

摘要

月球0.053的不可忽略的轨道偏心率的起源尚无理论解释。月球激光测距表明,地球的潮汐目前正在增加月球的偏心率。然而,在最初的10亿年里,海洋潮汐可能要弱得多,使得月球潮汐在很早的时候就消除了任何原始的月球偏心率。在其轨道由潮汐驱动的扩张过程中,月球必定受到了与木星和金星相关的两个显著共振的影响,通过这些共振可能产生了如今月球的偏心率。

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引用本文的文献

1
Tidal evolution of the Moon from a high-obliquity, high-angular-momentum Earth.月球从高倾斜度、高角动量的地球潮汐演化而来。
Nature. 2016 Nov 17;539(7629):402-406. doi: 10.1038/nature19846. Epub 2016 Oct 31.
2
Tidal Venuses: triggering a climate catastrophe via tidal heating.潮汐金星:通过潮汐加热引发气候灾难。
Astrobiology. 2013 Mar;13(3):225-50. doi: 10.1089/ast.2012.0851.