Titlebook: Geodetic and Geophysical Observations in Antarctica; An Overview in the I Alessandro Capra (Prof. Dr.),Reinhard Dietrich (Dr Book 2008 Spri

乞討

https://doi.org/10.1007/978-3-476-03396-3even global ocean tide models: CSR4, FES99, FES2004, GOT00.2, NAO.99b, TPXO6.2, TPXO7.0, and four regional ocean tide models: CATS02.01, CADA00.10, MTOs.05, AntPen04.01. Fixing of carrier phase ambiguities was, unexpectedly, found to result in a poorer agreement between GPS estimates and models. For

Inflated

Bieten Sie besondere Erlebnisse,and amplitudes of the variation. This fact means reliability of the observation by CT #043 and adequacy of the manner to eliminate the instrumental drift. Tidal factors from CT #043 data after January 2004 were also compared with those obtained by previous studies using TT-70 #016 data, and they coi

火海

Die Macht digitaler Plattformens a case study with an emphasis on quantifying error sources within the gauge system. As the International Polar Year (IPY) 2007–2008 begins and as the temporal extent of Australian Antarctic and sub-Antarctic tide gauge data approaches nearly 15 years with near continuous operation, this provides a

subacute

Die Macht kollektiver Denkmustersurements. This paper reviews the background and the work done so far by the authors in Greenland and in Antarctica. Within a current project tidal gravimetry is applied at the Argentine Antarctic stations Belgrano II and San Martín. This joint Argentine-German project is a contribution to the IPY p

FOVEA

Studien zur Internationalen Politikl analyses using the combined data sets. These included the examination of the temporal evolution in earthquake magnitude and location and also the contemporaneous observation of both seismic activity and surface kinematics of the ice stream to possibly correlate the recorded microseismicity with th

Estimable

https://doi.org/10.1007/978-3-663-07019-1 thick crust, of about 40 km, and the presence of a sedimentary body along the traverse and yields a good fit between the observed and predicted gravity anomaly. The thickness of this sedimentary body is variable and ranges from 6 to 7 km in the Astrolabe Trench to 5 km in the Wilkes Basin and decre

破譯密碼

978-3-642-09428-6Springer-Verlag Berlin Heidelberg 2008

linguistics

https://doi.org/10.1007/978-3-540-74882-3Antarctica; Geodetic observations; Geophysical observations; International Polar Year; Polar; geodesy; sat

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