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Titlebook: Geodynamics and Earth Tides Observations from Global to Micro Scale; Carla Braitenberg,Giuliana Rossi,Geodynamics and E Book 2019 Springer

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發(fā)表于 2025-3-21 19:19:58 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Geodynamics and Earth Tides Observations from Global to Micro Scale
編輯Carla Braitenberg,Giuliana Rossi,Geodynamics and E
視頻videohttp://file.papertrans.cn/384/383122/383122.mp4
叢書名稱Pageoph Topical Volumes
圖書封面Titlebook: Geodynamics and Earth Tides Observations from Global to Micro Scale;  Carla Braitenberg,Giuliana Rossi,Geodynamics and E Book 2019 Springer
描述This volume treats the key aspects that must be known when dealing with continuous space geodetic or terrestrial geodetic observations. The signals of Earth core resonance are discussed, as well as tidal effects on Earth polar motion and on earthquake triggering. Hydrologic loading, be it ocean tides or subsurface water flows, is discussed. These signals compete with crustal deformation observations of earthquakes (e.g., Gorkha 2015) during interseismic periods, and on volcanoes (Elbrus, Caucasus). The instrumentation that is covered includes superconducting gravimeters, continuous seafloor gravimeters, interferometric tilt? and strain meters, and GNSS networks..The articles give an up-to-date account of research in which the Earth tides are a benchmark signal for the sophisticated instrumentation mounted on satellites or the surface, observing time-variable signals of an evolving Earth. Scientists studying the earthquake cycle and geodetic monitoring will find useful material.For students in the geosciences, the collection offers a good overview of the broad spectrum of topics related to the Earth geodetic monitoring..
出版日期Book 2019
關(guān)鍵詞earth tides; ocean loading tides; polar motion; ut1; earth core resonance; superconducting gravimeters; gn
版次1
doihttps://doi.org/10.1007/978-3-319-96277-1
isbn_softcover978-3-319-96276-4
isbn_ebook978-3-319-96277-1Series ISSN 2504-3625 Series E-ISSN 2504-3633
issn_series 2504-3625
copyrightSpringer Nature Switzerland AG 2019
The information of publication is updating

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發(fā)表于 2025-3-21 22:49:11 | 只看該作者
Maschinenteile der drehenden Bewegung,ndently of correction of the strain data. These discrepancies need further investigations. According to our results, fluid core resonance effects can also be detected by our quartz tube extensometers but correction of strain data for local effects is necessary.
板凳
發(fā)表于 2025-3-22 02:17:24 | 只看該作者
地板
發(fā)表于 2025-3-22 04:55:16 | 只看該作者
Die Zwischen- und Abdampfverwertungfference in the seasonal gravity variations of OSG- 073 and T020. We have found clear gravity differences due to transient effect of heavy precipitation. In addition, we compare the remote effect on gravity due to variations in the Baltic Sea level and total water storage in Finland to the observed
5#
發(fā)表于 2025-3-22 09:35:05 | 只看該作者
https://doi.org/10.1007/978-3-662-33178-1ghtly higher than that of independent component analysis (ICA). EMD-ICA could overcome the limitation of ICA having to process multiple observations and slightly improve the extraction accuracy and reliability of gravity tides from relative gravimeter data compared to that estimated with ICA.
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發(fā)表于 2025-3-22 15:01:41 | 只看該作者
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發(fā)表于 2025-3-22 18:03:30 | 只看該作者
,Der Kompromi?charakter der Entfremdung,ile at higher frequencies strain noise is higher than at Kamioka, Japan, probably because of frequency instabilities of the laser source. Environmental (air temperature and pressure) effects on measured strain are quite small; thus, signal-to-noise ratio in the tidal bands is unusually high. In part
8#
發(fā)表于 2025-3-22 22:11:23 | 只看該作者
https://doi.org/10.1007/978-3-662-26162-0 of 7% of the RMS is obtained. The wavelet transform is applied to the same series, before and after the nontidal correction, and a clear decrease in the spectral energy in the periods between 2 and 12 days is identify between the series. Using the same software East, North and Up displacements are
9#
發(fā)表于 2025-3-23 04:57:04 | 只看該作者
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發(fā)表于 2025-3-23 09:21:29 | 只看該作者
https://doi.org/10.1007/978-3-658-33665-3 series of the river and the data recorded by multiparametric loggers. Additionally, the data of a permanent GPS station located on the southern slopes of the Cansiglio Massif (CANV) show also a clear correspondence with the river level. The fast water infiltration into the epikarst, closely related
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