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Intercomparison of Lunar Laser and Traditional Determinations of Earth Rotation

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Part of the book series: Astrophysics and Space Science Library ((ASSL,volume 94))

Abstract

The rotational orientation of the earth (UTO at McDonald Observatory) has been determined from lunar laser ranging (LLR) measurements for the interval 1971 to 1980. The results have been differenced from those obtained by conventional means as published by the Bureau International de l’Heure (BIH), on its 1979 system. The difference displays a quasi-seasonal signature, which we ascribe to systematic errors in the conventional measurements. The lunar data are well represented by a smooth curve, which gives UTO at McDonald with a precision of about 3/4 milliseconds or better, and UT1 to within 1 millisecond using BIH polar coordinates.

The amplitude spectrum of the UT1 differences (LLR-BIH) displays highest values at low frequencies, and diminishes toward higher frequencies until a white noise regime is reached for periods of 70 days or less. This suggests that a moderately smoothed version of UT1, corresponding to a Gaussian filter of the form exp{−t2/2σ2} with σ = 10 or 12 days, will usually be a good representation of Earth rotation. However, there appear to be short episodes of high acceleration revealed by the LLR data, showing that there are intervals during which frequent observation is scientifically valuable.

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© 1982 D. Reidel Publishing Company

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Fliegel, H.F., Dickey, J.O., Williams, J.G. (1982). Intercomparison of Lunar Laser and Traditional Determinations of Earth Rotation. In: Calame, O. (eds) High-Precision Earth Rotation and Earth-Moon Dynamics. Astrophysics and Space Science Library, vol 94. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-7807-2_6

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  • DOI: https://doi.org/10.1007/978-94-009-7807-2_6

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-009-7809-6

  • Online ISBN: 978-94-009-7807-2

  • eBook Packages: Springer Book Archive

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