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  • 1
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Gravity -- Measurement. ; Satellite geodesy. ; Geodetic satellites. ; Electronic books.
    Description / Table of Contents: In Germany, many processing, modeling and interpreting methodologies for studying the earth's magnetic and gravity fields were developed under a specific program using satellites. This book presents results of studies in that program from 2005-2008.
    Type of Medium: Online Resource
    Pages: 1 online resource (586 pages)
    Edition: 1st ed.
    ISBN: 9783642102288
    Series Statement: Advanced Technologies in Earth Sciences Series
    Language: English
    Note: Intro -- Preface -- Contents -- Contributors -- Part I CHAMP and GRACE -- More Accurate and Faster Available CHAMP and GRACE Gravity Fields for the User Community -- 1 Introduction -- 2 Gravity Field Determination from Analysis of High-Low SST Data -- 3 Main Results of the BMBF/DFG Project CHAMP/GRACE -- References -- The CHAMP/GRACE User Portal ISDC -- 1 Introduction -- 2 Data Lifecycle Management -- 3 Metadata Model -- 4 Portal Architecture -- 4.1 Application Framework -- 4.2 Data Flow -- 4.3 Interfaces -- 5 Backend for Operational Services -- 5.1 Component Deployment -- 6 Outlook -- References -- Improvements for the CHAMP and GRACE Observation Model -- 1 Introduction -- 2 GPS Carrier Phase Wind-Up -- 2.1 General -- 2.2 Carrier Phase Wind-Up Validation -- 3 GPS Attitude Model -- 3.1 Nominal Yaw Regime -- 3.2 Noon/Midnight Turn Regime -- 3.3 Shadow Crossing Regime -- 3.4 Post-shadow Regime -- 4 Summary -- References -- The Release 04 CHAMP and GRACE EIGEN Gravity Field Models -- 1 Introduction -- 2 Monthly EIGEN-GRACE05S Time Series -- 3 Weekly EIGEN-GRACE05S Time Series -- 4 Monthly EIGEN-CHAMP05S Time Series -- 5 Satellite-Only and Combined EIGEN-5S and EIGEN-5C Solutions -- 6 A New Mean, Static EIGEN-CHAMP05S Gravity Field Model and Its Evaluation -- 7 Summary and Conclusions -- References -- Orbit Predictions for CHAMP and GRACE -- 1 Introduction -- 2 Orbit Prediction System -- 2.1 Preprocessing -- 2.2 Orbit Determination -- 2.3 Products -- 3 Accuracy of Predicted Orbits -- 4 Conclusions -- References -- Rapid Science Orbits for CHAMP and GRACE Radio Occultation Data Analysis -- 1 Introduction -- 2 GPS Rapid Science Orbits -- 3 Low Earth Orbiters Rapid Science Orbits -- 4 Summary -- References -- Parallelization and High Performance Computationfor Accelerated CHAMP and GRACE Data Analysis -- 1 Introduction. , 2 Removal of GPS Clock Parameters from the Observation Equations Using Dedicated Projections -- 3 Accelerated Computation of Normal Equations from Observation Equations via Additional Row-Block Parallelization -- 4 Adjustment of Satellite Arcs of Arbitrary Length -- 5 Conclusion -- References -- Part II GRACE -- Improved GRACE Level-1 and Level-2 Productsand Their Validation by Ocean Bottom Pressure -- 1 Introduction -- 2 The GRACE Mission Configuration and Key Instrumentation -- 3 The GRACE Level-1 and Level-2 Products -- 4 Main Results of the BMBF/DFG Project GRACE -- References -- The GRACE Gravity Sensor System -- 1 GRACE Sensor System -- 1.1 The Accelerometer -- 1.1.1 Logical Model -- 1.1.2 Accelerometer Noise Model -- 1.2 The Star Sensor -- 1.2.1 Star Sensor Noise Model -- 1.3 The GPS Receiver -- 1.3.1 Error Model -- 1.4 The K-Band Ranging System -- 1.4.1 Error Model -- 2 Sensor System Interaction -- 3 Force Models -- 3.1 Gravitational Forces -- 3.2 Non-gravitational Forces -- 4 Real Data Analysis -- 5 Data Processing -- 6 Conclusions and Outlook -- References -- Numerical Simulations of Short-Term Non-tidal Ocean Mass Anomalies -- 1 Introduction -- 2 Ocean Model for Circulation and Tides (OMCT) -- 3 ECMWF Analyses and Forecasts -- 4 Continental and Atmospheric Freshwater Fluxes -- 5 Variations in Total Ocean Mass -- 6 Conclusions -- References -- Improved Non-tidal Atmospheric and Oceanic De-aliasing for GRACE and SLR Satellites -- 1 Introduction -- 2 OMCT Configuration for AOD1B RL04 -- 3 Increase of the Temporal Resolution of AOD1B -- 4 AOD1B RL04 Time Series for Consistent SLR Data Processing -- 5 Conclusions -- 6 Notes -- References -- Global Gravity Fields from Simulated Level-1 GRACE Data -- 1 Introduction -- 2 Simulation of Observations -- 3 Estimation of Arc Specific Parameters and Gravity Field Coefficients. , 4 Estimation of Instrument Parameters -- 5 Orbit Geometry and Omission Error -- 6 Effect of Errors in the Background Models -- 7 Colored Observation Noise -- 8 Variation of the Arc Length and the Number of Instrument Parameters -- 9 Special Experiments Concerning the C20 Coefficient -- 10 Summary and Conclusions -- References -- ITG-GRACE: Global Static and Temporal Gravity Field Models from GRACE Data -- 1 Introduction -- 2 Physical Model -- 2.1 Model Setup -- 2.2 Stochastic Model -- 2.3 Representation of the Gravity Field -- 2.3.1 Static Gravity Field Representation -- 2.3.2 Representation of the Time Variable Gravity Field -- 3 Gravity Field Solution ITG-Grace03s -- 3.1 Data Set and Estimated Parameters -- 3.2 Temporal Variations -- 3.3 Static Solution -- 3.4 Covariance-Matrix -- 4 Conclusions -- References -- Validation of GRACE Gravity Fields by In-Situ Data of Ocean Bottom Pressure -- 1 Introduction -- 2 Data -- 2.1 In-Situ Ocean Bottom Pressure -- 2.2 GRACE -- 3 Methods -- 4 Results -- 5 Summary and Conclusions -- References -- Antarctic Circumpolar Current Transport Variability in GRACE Gravity Solutions and Numerical Ocean Model Simulations -- 1 Introduction -- 2 Data -- 3 Transport Variability and Ocean Bottom Pressure -- 4 SAM in GRACE Ocean Bottom Pressure -- 5 Discussion -- References -- Part III GOCE -- Gravity and Steady-State Ocean Circulation Explorer GOCE -- 1 Introduction -- 2 The GOCE Mission -- 3 GOCE in the Context of the Geotechnology-Programme -- 4 Conclusions -- References -- GOCE Data Analysis: From Calibrated Measurementsto the Global Earth Gravity Field -- 1 Introduction -- 2 Processing Strategy for the Different Data Types -- 2.1 Processing of the SST Data -- 2.1.1 Kinematic Orbit and Velocity Determination -- 2.1.2 Energy Integral -- 2.2 Processing of the SGG Data -- 2.2.1 Functional Model for In-Situ SGG Data Processing. , 2.2.2 Stochastic Model of SGG Data -- 2.3 Introduction of Regularizing Prior Information -- 2.4 Combination of All Observation Groups -- 3 Solving the Combined Normal Equation System -- 3.1 Preconditioned Conjugate Gradients Multiple Adjustment -- 3.2 Integration of VCE into PCGMA -- 3.3 Integration of the Decorrelation Filters into PCGMA -- 4 Conclusion and Outlook -- References -- GOCE and Its Use for a High-Resolution Global Gravity Combination Model -- 1 Pre-GOCE Satellite-only Models -- 2 GOCE and Satellite-only Models -- 3 GOCE and Global Gravity Field Combination Models -- 3.1 Surface Data -- 3.2 Combination Models Derived from Full and Block-Diagonal Normal Equations -- 3.3 The GOCE-Model: Combination with Full Normal Equations Only -- 4 Conclusions -- References -- Spectral Approaches to Solving the Polar Gap Problem -- 1 Introduction -- 2 Selected Strategies A Review -- 2.1 Stabilization with External Data -- 2.2 Stabilization without External Data -- 3 Regularization and Combination -- 4 Slepian Parameterization -- 4.1 Solving the Eigenvalue Problem -- 5 Conclusions -- References -- Regionally Refined Gravity Field Models from In-Situ Satellite Data -- 1 Introduction -- 2 Mathematical Model -- 2.1 Basis Functions -- 2.2 Regionally Adapted Regularization -- 3 Simulation Scenario -- 4 Conclusions -- References -- Quality Evaluation of GOCE Gradients -- 1 Cross-Over Analysis -- 1.1 Short Term Biases -- 1.2 Trend -- 1.3 Fourier Coefficients -- 2 Accuracy Analysis of External Reference Gradients in the Frequency Domain -- 2.1 Spectral Combination Method -- 2.2 Synthetic Data -- 2.3 Closed-Loop Differences in the Frequency Domain -- 3 Generation of Quality Reports -- 4 Conclusions -- References -- Validation of Satellite Gravity Field Models by Regional Terrestrial Data Sets -- 1 Introduction -- 2 Gravity Data -- 3 GPS and Levelling Data. , 4 Gravimetric Quasigeoid Models -- 5 Astrogeodetic Vertical Deflections -- 5.1 Astrogeodetic Validation of GPS/Levelling Data and Gravimetric Quasigeoid Models -- 5.2 Astrogeodetic Validation of Global Geopotential Models -- 6 Global Model Validation by Wavelet Techniques -- 6.1 Filtering Terrestrial Data by Second Generation Wavelets -- 6.2 First Results with Second Generation Wavelets -- 7 Conclusions -- References -- Comparison of GRACE and Model-Based Estimates of Bottom Pressure Variations Against In Situ Bottom Pressure Measurements -- 1 Introduction -- 2 Methodology -- 3 Comparison of Results with Bottom Pressure Sensors -- 4 Comparison of GRACE Results with Model Simulations and Bottom Pressure Sensors -- 5 Global EOF Fields of GRACE and Model pb Variations -- 6 Concluding Remarks -- References -- Part IV SEAVAR -- Sea Level Variations -- Prospects from the Past to the Present(SEAVAR) -- Radar Altimetry Derived Sea Level Anomalies -- The Benefit of New Orbits and Harmonization -- 1 Introduction -- 2 The Altimeter Database and Processing System (ADS) -- 3 Harmonization of Different Altimetric Missions -- 4 The Effects of New Orbits -- 5 Summary and Outlook -- References -- Combining GEOSAT and TOPEX/Poseidon Data by Means of Data Assimilation -- 1 Introduction -- 2 Model and Data -- 3 Results -- 4 Summary and Conclusions -- References -- Reanalysis of GPS Data at Tide Gauges and the Combination for the IGS TIGA Pilot Project -- 1 Introduction -- 2 Reprocessing of GPS Data at Tide Gauge Benchmarks at GFT -- 3 Combination of Weekly TIGA Solutions -- 4 Summary and Conclusions -- References -- Sea Level Rise in North Atlantic Derived from Gap Filled Tide Gauge Stations of the PSMSL Data Set -- 1 Introduction -- 2 The PSMSL Gauge Data Set -- 3 Theoretical Background and Used Method -- 4 Reduced Number of Gauges and Calibration of IFEOM. , 5 Conclusions.
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  • 2
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: CHAMP (Artificial satellite) -- Congresses. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (642 pages)
    Edition: 1st ed.
    ISBN: 9783540268000
    DDC: 531.14
    Language: English
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  • 3
    Keywords: Forschungsbericht ; Klima ; Modell ; Satellitengeodäsie ; Validierung
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (20 Seiten, 2,85 MB) , Illustrationen, Diagramme
    Language: German
    Note: Förderkennzeichen BMBF 01LP1151A , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden
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  • 4
    Keywords: Forschungsbericht
    Description / Table of Contents: GPS, CHAMP, troposhere, ionosphere, water vapor, limb sounding, weather forecast, electron density, temperature, remote sensing
    Type of Medium: Online Resource
    Pages: Online-Ressource (66 S., 4,73 MB) , Ill., graph. Darst
    Language: German , English
    Note: Förderkennzeichen BMBF 01SF9921/23. - Engl. Titel: GPS Atmosphere Sounding Project (GASP) - an innovative approach for the recovery of atmospheric parameters. - Literaturangaben , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden , Auch als gedr. Ausg. vorh , Systemvoraussetzungen: Acrobat reader.
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  • 5
    Keywords: Forschungsbericht
    Type of Medium: Online Resource
    Pages: Online-Ressource (49 S., 2,43 MB) , Ill., graph. Darst.
    Language: German
    Note: Förderkennzeichen BMBF 03F0431 A , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden , Auch als gedr. Ausg. vorhanden , Systemvoraussetzungen: Acrobat reader.
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  • 6
    Publication Date: 2023-09-01
    Type: Dataset
    Format: application/zip, 11.5 MBytes
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  • 7
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    PANGAEA
    In:  Supplement to: Wang, Jungang; Wu, Zhilu; Semmling, Maximilian; Zus, Florian; Gerland, Sebastian; Ramatschi, Markus; Ge, Maorong; Wickert, Jens; Schuh, Harald (2019): Retrieving Precipitable Water Vapor From Shipborne Multi‐GNSS Observations. Geophysical Research Letters, 46(9), 5000-5008, https://doi.org/10.1029/2019GL082136
    Publication Date: 2023-10-28
    Description: The Multi-GNSS observations from an onboard receiver were retrieved using kinematic Precise Point Positioning (PPP) method. The solution using only Global Positioning System (GPS) observations is the GPS-only solution; and the one using GPS, GLONASS, and Galileo observations together, is the GRE PPP solution. R is short for the Russian system GLONASS, and E is short for Europe system Galileo. The GNSS data was collected by a GNSS receiver on R/V Lance. It is used by the Norwegian Polar Institute (NPI) for regular monitoring and research related to ocean and sea ice properties in Fram Strait. During the Fram Strait 2016 cruise from day-of-year (DOY) 238 to DOY 257, a geodetic JAVAD TR_G3TH GNSS receiver was installed on the ship bow, which is about 6 m above the water surface. This receiver collected multi-GNSS data at a sampling of 1-Hz, including GPS, GLONASS, and Galileo.
    Keywords: cruise_57; CT; DATE/TIME; Day of the year; ECMWF; Fram Strait; GNSS; LA1608; LA1608-track; Lance; LATITUDE; LONGITUDE; Precipitable water vapour; Precise Point Positioning (PPP); PWV; SARAL; Underway cruise track measurements; Zenith total delay
    Type: Dataset
    Format: text/tab-separated-values, 283550 data points
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  • 8
    Publication Date: 2019-08-05
    Description: A numerical algorithm based on Fermat's Principle was developed to simulate the propagation of Global Positioning System (GPS) radio signals in the refractivity field of a numerical weather model. The unique in the proposed algorithm is that the ray-trajectory automatically involves the location of the ground-based receiver and the satellite, i.e. the posed two-point boundary value problem is solved by an implicit finite difference scheme. This feature of the algorithm allows the fast and accurate computation of the signal travel-time delay, referred to as Slant Total Delay (STD), between a satellite and a ground-based receiver. We provide a technical description of the algorithm and estimate the uncertainty of STDs due to simplifying assumptions in the algorithm and due to the uncertainty of the refractivity field. In a first application, we compare STDs retrieved from GPS phase-observations at the German Research Centre for Geosciences Potsdam (GFZ STDs) with STDs derived from the European Center for Medium-Range Weather Forecasts analyses (ECMWF STDs). The statistical comparison for one month (August 2007) for a large and continuously operating network of ground-based receivers in Germany indicates good agreement between GFZ STDs and ECMWF STDs; the standard deviation is 0.5% and the mean deviation is 0.1%.
    Type: Article , PeerReviewed
    Format: text
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  • 9
    Publication Date: 2014-12-09
    Description: Water vapor plays an important role in meteorological applications; GeoForschungsZentrum (GFZ) therefore developed a tomographic system to derive 3-D distributions of the tropospheric water vapor above Germany using GPS data from about 300 ground stations. Input data for the tomographic reconstructions are generated by the Earth Parameter and Orbit determination System (EPOS) software of the GFZ, which provides zenith total delay (ZTD), integrated water vapor (IWV) and slant total delay (STD) data operationally with a temporal resolution of 2.5 min (STD) and 15 min (ZTD, IWV). The water vapor distribution in the atmosphere is derived by tomographic reconstruction techniques. The quality of the solution is dependent on many factors such as the spatial coverage of the atmosphere with slant paths, the spatial distribution of their intersections and the accuracy of the input observations. Independent observations are required to validate the tomographic reconstructions and to get precise information on the accuracy of the derived 3-D water vapor fields. To determine the quality of the GPS tomography, more than 8000 vertical water vapor profiles at 13 German radiosonde stations were used for the comparison. The radiosondes were launched twice a day (at 00:00 UTC and 12:00 UTC) in 2007. In this paper, parameters of the entire profiles such as the wet refractivity, and the zenith wet delay have been compared. Before the validation the temporal and spatial distribution of the slant paths, serving as a basis for tomographic reconstruction, as well as their angular distribution were studied. The mean wet refractivity differences between tomography and radiosonde data for all points vary from −1.3 to 0.3, and the root mean square is within the range of 6.5–9. About 32% of 6803 profiles match well, 23% match badly and 45% are difficult to classify as they match only in parts.
    Type: Article , PeerReviewed
    Format: text
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  • 10
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