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Titlebook: Earth Rotation: Solved and Unsolved Problems; Anny Cazenave Book 1986 D. Reidel Publishing Company, Dordrecht, Holland. 1986 Variation.atm

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发表于 2025-3-21 17:31:13 | 显示全部楼层 |阅读模式
书目名称Earth Rotation: Solved and Unsolved Problems
编辑Anny Cazenave
视频videohttp://file.papertrans.cn/301/300846/300846.mp4
丛书名称Nato Science Series C:
图书封面Titlebook: Earth Rotation: Solved and Unsolved Problems;  Anny Cazenave Book 1986 D. Reidel Publishing Company, Dordrecht, Holland. 1986 Variation.atm
描述The idea for organl.zl.ng an Advanced Research Workshop entirely devoted to the Earth rotation was born in 1983 when Professor Raymond Hide suggested this topic to the special NATO panel of global transport mechanism in the Geosciences. Such a specialized meeting did not take place since the GEOP research conference on the rotation of the Earth and polar motion which was held at the Ohio State University (USA) in 1973. In the last ten years, highly precise measurements of the Earth‘s rotation parameters and new global geophysical data have become available allowing major advance to be made in the under­ standing of the various irregularities affecting the Earth‘s rotation. The aim of the workshop was to bring together scientists who have made important contributions in this field during the last decade both at the observational and geophysical interpretation levels. The confe­ rence was divided into four main topics. The first session was dedicated to the definition, implementation and maintenance of the terrestrial and celestial reference systems. A few critical points have been identified as requiring further improvements: (i) appro­ priate selection of terrestrial sites recogniz
出版日期Book 1986
关键词Variation; atmosphere; dynamics; earth; oscillation; solar activity; stability
版次1
doihttps://doi.org/10.1007/978-94-009-4750-4
isbn_softcover978-94-010-8610-3
isbn_ebook978-94-009-4750-4Series ISSN 1389-2185
issn_series 1389-2185
copyrightD. Reidel Publishing Company, Dordrecht, Holland. 1986
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发表于 2025-3-21 21:36:51 | 显示全部楼层
The Conceptual and Conventional Definitions of the Earth Rotation Parametersessary to define these parameters with the same order of precision. In this purpose, the conceptual definitions (Eichhorn 1983) which should be used for the ERP are given as well as the conventional definitions corresponding to the geometrical or dynamical principles involved in the various methods
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Polar Motion and Signal Processingts. After recall of the basic equation of motion and its solution, the most usual methods are surveyed with emphasis on the frequently implicit hypotheses. The 1900 –1977 ILS series is used to apply a simple variable spectral analysis. In addition the Fourier transform restricted to the 1967 –1984 B
发表于 2025-3-22 09:36:33 | 显示全部楼层
Accurate Earth Orientation time Series from vlbi Observationsprecession. The IRIS polar motion time series comprises x and y values at 5-day intervals with accuracies, verified by intercomparisons with SLR values, of better than 2 milliseconds of arc. The UT1 series includes values at 5-day intervals with estimated accuracies of 0.05 to 0.10 millisecond, and
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Tidal and non Tidal Acceleration of the Earth’s Rotationto UT and several solutions where the rate of change of the length of the day was determined simultaneously with the secular acceleration of the Moon mean longitude. Quite recently it has been possible to rely on independent measurements of n, the value of which has become central in studies of the
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Global Climatic Changes and Astronomical Theory of Paleoclimatessuccession of Pleistocene Ice Ages. Spectral analysis of geo-climatic records of the past 800,000 years has provided substantial evidence that a considerable fraction of the climatic variance is driven, in some way, by insolation changes accompagnying changes in the Earth’s orbit, at least near the
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Meteorological Data for Earth Rotation Studiestity produced by two operational weather centers. The two series generally agree quite well, although certain differences are evident and discussed here. The effect of neglecting middle and upper stratospheric winds in the production of these series is also considered and shown to be of some consequ
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