Every four years the International Association of Geodesy meets at the IUGG General Assembly and this has always been an important event for IAG to make the point on where are we going as geodesists both in terms of scientific production as well as in terms of organization. The proceedings of IAG at the Sapporo 2003 General Assembly are the mirror of our scientific achievements, and, as Geodesy is a living entity like any other science, we could say it is a way to see the picture of what we consider our field of applications as well as of theoretical speculations. Let us examine this aspect in terms of what are: the object of our research, the methods we use, the general scientific results we can produce. • Our object: here I would like to use a pseudo-Helmert definition; the object of Geodesy is knowing the surfaces of the earth: the geometric surface by positioning and e.m. surveying, and the physical surface, i.e the gravity field, by land, marine or satellite gravimetry, and their time variations. This "object" is naturally interlaced with other physical properties of the earth both through deep processes affecting its surface and through the gravity field at all different scales from the global to the regional and local, where most engineering applications take place.
"synopsis" may belong to another edition of this title.
This book collects the proceedings of the symposia held during the 36th IAG General Assembly. This international event, held every fourth year, serves as a forum to announce and record new achievements and the primary research directions of the worldwide geodetic community. The actual date of this assembly, on the verge of the 3rd millennium, adds a particular accent to the results and proposals collected here, which is especially exemplified by the new perspectives derived by the advanced tools and techniques of earth observation from space platforms. Not to be overlooked are the enhanced capabilities of the now classic navigation and positioning systems, under the collective name GNSS. Together with classic techniques like SLR, VLBI, Doris, Prare etc., these provide the capability for establishing a global reference frame at the millimeter level, which currently relates global with regional phenomena of the physics of the earth. In recent years, the surface of the earth has been surveyed with a SAR technique covering all the continents, while the ocean is continuously monitored by new altimetric missions.
Furthermore, the gravity field is now measured from space and interpreted in terms of geodynamical phenomena. Even more accurate and high resolution missions are planned, the study of which has already strongly propelled new theoretical achievements in the field of gravity modeling. All this is contained in these proceedings, opening a window to the future of all these promising and exciting developments."About this title" may belong to another edition of this title.
Seller: killarneybooks, Inagh, CLARE, Ireland
Hardcover. Condition: Very Good. Oversized hardcover, xvii + 619 pages, NOT ex-library. Weight 1700g. Clean and bright throughout with unmarked text, free of inscriptions and stamps. Signs of light wear. Issued without a dust jacket. -- Contents (a selection): 1 Positioning [ITRF Combination; Time Evolution of Terrestrial Reference Frame; Scale Variation of GPS Time series; Vertical Repeatability of GPS Measurements in Tsukuba GPS/MET Dense-Network Campaigns; Horizontal Crustal Motion Estimates for the UK Inferred from GPS; Results of the SIRGAS Campaign 2000.; Implementation of Semi-Dynamic Datum: New Zealand; Why GPS Is Less Accurate in Mountain Areas; More Reliable Estimation of GPS Positioning Accuracy; Realistic Uncertainty Measures: GPS Observations; Networked Transport of RTCM via Internet Protocol NTRIP; Numerical Weather Predictions: GPS Positioning; Multi-Base-Station Approach for Long Range Differential GNSS Positioning of Airborne Sensors; Point Real-Time Kinematic Positioning; Integration of GPS & Pseudolites: Bridge Monitoring; Hybrid Sensor System for Bridge Deformation Monitoring; Fuzzy System: Assessment of Landslide Monitoring Data; OASYS: Integrated Optimization of Landslide Alert Systems; Combined Evaluation of Geodetic & Geotechnical Data during Tunnel Excavation: Knowledge-Based System]; 2 Advanced Space Technology [Quasi Real-Time Positioning of Spacecrafts: Internet VLBI System; Rapid Turnaround EOP Measurements by VLBI over the Internet; Determination of Tropospheric Parameters: New IVS Pilot Project; Vlbionos: Probing the Ionosphere by Means of Very Long Baseline Interferometry; Numerical Simulations for Geodetic Parameter Estimation from Space VLBI Data; Relativistic VLBI Delay Model for Finite Distance Radio Source; Synergy of VLBI & GPS Observations in Japan; Ground-Based Verification of 4-Way Doppler Measurement: SELENE mission; Results of the Critical Design of RSAT/VRAD Mission Instruments on SELENE Sub-Satellites Rstar/Vstar for Selenodesy; PZT Telescope: In situ Lunar Orientation Measurement ILOM; Combined Processing of GPS Data from Ground Station & LEO Receivers in a Global Solution; Efficient Stochastic Orbit Modeling Techniques: Least Squares Estimators; Kinematic Precise Orbit Determination: Gravity Field Determination; Gravity Field Recovery & Validation by Analysis of Short Arcs of a Satellite-to-Satellite Tracking Experiment as CHAMP & GRACE; Combination of Sea-Level Observations and an Oceanographic Model: Baltic Sea Geodetic Applications; Analysis of GPS Campaign Observations: Asia Pacific Regional Geodetic Project APRGP; Proposed International DORIS Service; Calibration/Validation of GOCE Data: Terrestrial Torsion Balance Observations]; 3 Gravity Field Determination: - Gravimetry & Gravity Instrumentation [Repeated Measurements of Gravity with the Absolute Gravimeter FG5 #210 & Comparison with the Superconducting Gravimeter T011; Gravimetry by Helicopter to Identify Marine Active Faults & Improve Accuracy of Geoid: Coastal Zones; Gravity Database of Southwest Japan: Bouguer Gravity Imaging; Gravity-Based Fault Mapping; Compilation & Evaluation of Consistent Marine Gravity Data Set Surrounding Europe; Comparison of Downward Continuation Methods of Airborne Gravimetry Data; Optimisation of Density Parameter: Gravity Prediction from Bathymetry] - Gravity Satellite Missions: Data Processing & Applications - Satellite Altimetry for Gravity, Geoid & SST - Heights & Vertical Datums - Geoid Modelling; 4 General Theory & Methodology; 5 Geodynamics: - Applications of GPS to Crustal Deformation - Gravity Applications - Earth Rotation and Geodynamics Techniques; 6 Insight into Earth System Science: Variations in the Earth's Rotation & Its Gravity Field: - Earth Rotation Interpretation - Theoretical Studies Related to Earth Rotation & Time Variable Gravity; Author & Keyword Index. Seller Inventory # 004537
Seller: BuchWeltWeit Ludwig Meier e.K., Bergisch Gladbach, Germany
Buch. Condition: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -These proceedings represent the worldwide picture of the state of the art of geodesy. The volume comprehensively covers the most recent results and supplies a good review of the new ideas developing in the field, opening a window to the future of geodesy. 640 pp. Englisch. Seller Inventory # 9783540240556
Seller: AHA-BUCH GmbH, Einbeck, Germany
Buch. Condition: Neu. Druck auf Anfrage Neuware - Printed after ordering - Every four years the International Association of Geodesy meets at the IUGG General Assembly and this has always been an important event for IAG to make the point on where are we going as geodesists both in terms of scientific production as well as in terms of organization. The proceedings of IAG at the Sapporo 2003 General Assembly are the mirror of our scientific achievements, and, as Geodesy is a living entity like any other science, we could say it is a way to see the picture of what we consider our field of applications as well as of theoretical speculations. Let us examine this aspect in terms of what are: the object of our research, the methods we use, the general scientific results we can produce. - Our object: here I would like to use a pseudo-Helmert definition; the object of Geodesy is knowing the surfaces of the earth: the geometric surface by positioning and e.m. surveying, and the physical surface, i.e the gravity field, by land, marine or satellite gravimetry, and their time variations. This 'object' is naturally interlaced with other physical properties of the earth both through deep processes affecting its surface and through the gravity field at all different scales from the global to the regional and local, where most engineering applications take place. Seller Inventory # 9783540240556