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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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樓主: Johnson
41#
發(fā)表于 2025-3-28 15:50:29 | 只看該作者
Einführung in die Lineare Algebrasuccession 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
42#
發(fā)表于 2025-3-28 20:10:56 | 只看該作者
Franz-Josef Feldhege,Günter Krauthantity 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
43#
發(fā)表于 2025-3-29 00:04:50 | 只看該作者
Aufgaben über Zeitreihenanalysend their relation with changes in the global atmospheric angular momentum (AAM). Particular emphasis and attention are placed on data acquired during the MERIT campaign (September 1983 — October 1984). The modern space geodetic techniques have achieved unprecented accuracy and precision; intercompar
44#
發(fā)表于 2025-3-29 04:03:51 | 只看該作者
45#
發(fā)表于 2025-3-29 07:54:37 | 只看該作者
46#
發(fā)表于 2025-3-29 12:37:59 | 只看該作者
47#
發(fā)表于 2025-3-29 17:16:33 | 只看該作者
48#
發(fā)表于 2025-3-29 19:55:02 | 只看該作者
Earth Rotation: Solved and Unsolved Problems978-94-009-4750-4Series ISSN 1389-2185
49#
發(fā)表于 2025-3-30 02:21:44 | 只看該作者
https://doi.org/10.1007/978-3-322-94308-8Merit campaign allow to estimate the std. dev. of each techniques while their intercomparisons shows clearly the high quality of VLBI and SLR. However the other methods as Doppler and classical astronomy are still very valuable respectively for Polar Notion and UT. observations.
50#
發(fā)表于 2025-3-30 04:32:07 | 只看該作者
Franz-Josef Feldhege,Günter Krauthantity 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 consequence on seasonal time scales.
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