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發(fā)表于 2025-3-21 18:02:14 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Gravity, Geoid and Geodynamics 2000
編輯Michael G. Sideris
視頻videohttp://file.papertrans.cn/389/388262/388262.mp4
叢書名稱International Association of Geodesy Symposia
圖書封面Titlebook: ;
出版日期Conference proceedings 2002
版次1
doihttps://doi.org/10.1007/978-3-662-04827-6
isbn_softcover978-3-642-07634-3
isbn_ebook978-3-662-04827-6Series ISSN 0939-9585 Series E-ISSN 2197-9359
issn_series 0939-9585
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沙發(fā)
發(fā)表于 2025-3-21 21:05:06 | 只看該作者
板凳
發(fā)表于 2025-3-22 04:10:39 | 只看該作者
地板
發(fā)表于 2025-3-22 07:10:53 | 只看該作者
Error Analysis of the Gravity Recovery and Climate Experiment (GRACE) Missioncertain important error sources in these measurements, we describe the error simulation models. Effects of these error sources on gravity estimation are analyzed through a series of numerical simulations.
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發(fā)表于 2025-3-22 10:05:45 | 只看該作者
6#
發(fā)表于 2025-3-22 15:51:34 | 只看該作者
Adelaide Braga,Isabel Rocha,Nuno Faria Stokes’ integral to obtain an expression for the geoid undulation in a wavelet basis. An implementation is described and a geoid undulation map is produced. A technique to obtain a local update to both the wavelet EGM and the geoid undulations in regions where new gravity anomalies are available is described.
7#
發(fā)表于 2025-3-22 18:38:42 | 只看該作者
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發(fā)表于 2025-3-22 22:44:21 | 只看該作者
9#
發(fā)表于 2025-3-23 02:00:19 | 只看該作者
Global Unification of Height Systems and GOCE to give a global map of dynamic ocean topography, for the indirect method it serves the computation of reference geoid height differences. In both cases the off-sets between height datums will become estimable with a precision of a few centimetres.
10#
發(fā)表于 2025-3-23 07:09:34 | 只看該作者
A Wavelet Based Gravity Model with an Application to the Evaluation of Stokes’ Integral Stokes’ integral to obtain an expression for the geoid undulation in a wavelet basis. An implementation is described and a geoid undulation map is produced. A technique to obtain a local update to both the wavelet EGM and the geoid undulations in regions where new gravity anomalies are available is described.
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