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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(shū)目名稱(chēng)Geodetic and Geophysical Observations in Antarctica
副標(biāo)題An Overview in the I
編輯Alessandro Capra (Prof. Dr.),Reinhard Dietrich (Dr
視頻videohttp://file.papertrans.cn/384/383119/383119.mp4
概述Integrates data acquired in the field with observations in order to provide an understanding of the polar region environment.Provides a great overview on the advantages of the scientific utilization o
圖書(shū)封面Titlebook: Geodetic and Geophysical Observations in Antarctica; An Overview in the I Alessandro Capra (Prof. Dr.),Reinhard Dietrich (Dr Book 2008 Spri
描述.Due to their unique geophysical and geodynamic environment, both the Arctic and Antarctic polar regions are often utilized for geodetic and geophysical observations. This book is a collection of papers on various aspects of the scientific investigation and observation techniques of the polar regions at both temporary and permanent observatories. Most papers focus on regional models based on data acquired in polar regions. Geodetic satellite positions systems (GNSS: GPS, GLONASS, GALILEO) will also be discussed as well as other space techniques (DORIS, VLBI). Gravimetry, absolute gravimetry, and tidal gravimetry are also discussed, as well as seismology and meteorology. The book also touches on data analysis and geodynamic interpretation and discusses methods of constructing autonomous observatories..
出版日期Book 2008
關(guān)鍵詞Antarctica; Geodetic observations; Geophysical observations; International Polar Year; Polar; geodesy; sat
版次1
doihttps://doi.org/10.1007/978-3-540-74882-3
isbn_softcover978-3-642-09428-6
isbn_ebook978-3-540-74882-3
copyrightSpringer-Verlag Berlin Heidelberg 2008
The information of publication is updating

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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
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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
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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
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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
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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
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