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Titlebook: Earth on the Edge: Science for a Sustainable Planet; Proceedings of the I Chris Rizos,Pascal Willis Conference proceedings 2014 Springer-Ve

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樓主: 遮陽傘
31#
發(fā)表于 2025-3-26 22:13:41 | 只看該作者
https://doi.org/10.1007/978-1-349-06722-0rface waste repositories. Since November 2005 a high sensitive tilt meter of the ASKANIA-type is recording at a distance of 300 m from Mizunami Underground Research Laboratory, where two vertical shafts are under construction. During the construction of those shafts large pumps were used to reduce t
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發(fā)表于 2025-3-27 04:42:44 | 只看該作者
Conference proceedings 2014This book series is composed of peer-reviewed proceedings of selected symposia organized by the International Association of Geodesy. It deals primarily with topics related to Geodesy Earth Sciences : terrestrial reference frame, Earth gravity field, Geodynamics and Earth rotation, Positioning and engineering applications.
33#
發(fā)表于 2025-3-27 09:00:14 | 只看該作者
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發(fā)表于 2025-3-27 12:34:19 | 只看該作者
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發(fā)表于 2025-3-27 15:53:15 | 只看該作者
Zenith Wet Delay Retrieval Using Two Different Techniques for the South American Region and Their CoThe main purpose of the present work is to propose a comparison of the Zenith Wet Delay (ZWD) retrieved by GPS with the direct measurements provided by the water vapor radiometer loaded on-board the Jason-1 altimetry satellite and those obtained from SIRGAS (Geocentric Reference System for the Ameri
36#
發(fā)表于 2025-3-27 18:23:39 | 只看該作者
Mean Dynamic Ocean Topography in the Southern Ocean from GRACE and GOCE and Multi-mission Altimeter limate. We compute a high resolution mean dynamical ocean topography (MDT) using geodetic data and derive a detailed model of the global ocean circulation in this crucial area. The MDT is determined using multi-mission altimeter data and the GRACE/GOCE gravity model GOCO2s. The mean sea surface is o
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發(fā)表于 2025-3-28 00:51:58 | 只看該作者
38#
發(fā)表于 2025-3-28 02:34:27 | 只看該作者
Estimation of PGR Induced Absolute Gravity Changes at Greenland GNET Stationschanges in the relative sea-level (RSL). Several methods are used for mass balance studies but they are associated with large uncertainties. One reason for the uncertainty is the presence of the postglacial rebound (PGR) signal in the geodetic data used for mass balance estimates. Estimates of the P
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發(fā)表于 2025-3-28 09:56:29 | 只看該作者
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發(fā)表于 2025-3-28 12:10:17 | 只看該作者
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