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

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書目名稱Geodetic and Geophysical Observations in Antarctica影響因子(影響力)




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書目名稱Geodetic and Geophysical Observations in Antarctica網(wǎng)絡公開度學科排名




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書目名稱Geodetic and Geophysical Observations in Antarctica被引頻次學科排名




書目名稱Geodetic and Geophysical Observations in Antarctica年度引用




書目名稱Geodetic and Geophysical Observations in Antarctica年度引用學科排名




書目名稱Geodetic and Geophysical Observations in Antarctica讀者反饋




書目名稱Geodetic and Geophysical Observations in Antarctica讀者反饋學科排名

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Nonporous

GPS and Radiosonde Derived Precipitable Water Vapour Content and its Relationship with 5 Years of Liative effects on the thermal radiation balance of the atmosphere are of basic importance for the energy budget of the surface-atmosphere system in Antarctica, even though Precipitable Water assumes in general appreciably lower values than in other areas of our planet..Therefore, precise calculation

gorgeous

范圍廣

Continuous Gravity Observation with the Superconducting Gravimeter CT #043 at Syowa Station, Antarcand 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

范圍廣

Tide Gauges in the Antarctic and sub-Antarctic: Instrumentation and Calibration Issues from an Austs 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

GEAR

Tidal Gravimetry in Polar Regions: An Observation Tool Complementary to Continuous GPS for the Valisurements. 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

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Joint Geophysical Observations of Ice Stream Dynamics,l 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

獨行者

Structure of the Wilkes Basin Lithosphere along the ITASE01 Geotraverse, 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