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

奇怪

UNT

https://doi.org/10.1007/978-3-531-90383-5ones using FES2014b ocean model. Observed diurnal and semi-diurnal components are in good agreement with FES2014b predictions. Smallest constituents reflect some differences that may be attributed to non-linearity occurring at the Troll A site. Using the barotropic TUGO-m dynamic model of sea-level

出沒

討厭

Fester

A Filtering of Incomplete GNSS Position Time Series with Probabilistic Principal Component Analysis

原告

小鹿

Carla Braitenberg,Giuliana Rossi,Geodynamics and E

藐視

Long-Term Evaluation of Ocean Tidal Variation Models of Polar Motion and UT1,astic Earth model on the resulting ERP models. Our proposed alternative ERP model to the IERS 2010 conventional model considers the elastic model PREM and 260 partial tides. The choice of the ocean tide model and the determination of the tidal velocities have been identified as the main uncertaintie

Incommensurate

Observation of the Earth Liquid Core Resonance by Extensometers,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.

旋轉(zhuǎn)一周

Influence of Tidal Forces on the Triggering of Seismic Events,sults of calculations prove that stress increases as a function of depth reaching a value around some kPa at the depth of 900–1500 km, well below the zone of deep earthquakes. At the depth of the overwhelming part of seismic energy accumulation (around 50 km) the stresses of lunisolar origin are onl