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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
    Keywords: Forschungsbericht ; Indonesien ; Tsunami ; Frühwarnsystem ; Sonne
    Type of Medium: Online Resource
    Pages: Online-Resource (174 S.)
    Series Statement: IFM-GEOMAR-Report 5
    Language: English , German
    Note: Literaturverz. S. 129 - 131 , Zsfassungen in dt. u. engl. Sprache
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  • 3
    Keywords: Pacific Tsunami Warning and Mitigation System ; Natural disasters Research ; International cooperation ; Tsunamis Research ; Tsunamis Research ; Forschungsbericht ; Indonesien ; Tsunami ; Frühwarnsystem ; Sonne
    Type of Medium: Book
    Pages: 168 S. , Ill., graph. Darst., Kt.
    Series Statement: IFM-GEOMAR-Report 5
    DDC: 551.46/3715
    Language: English , German
    Note: Literaturverz. S. 129 - 131 , Auch als elektronisches Dokument vorh , Zsfassungen in dt. u. engl. Sprache
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  • 4
    Keywords: Hochschulschrift ; Forschungsbericht ; Weddellmeer ; Schwerefeld ; Weddellmeer ; Schwerefeld
    Type of Medium: Book
    Pages: VI, 145 S. , Ill., graph. Darst., Kt.
    Series Statement: Berichte zur Polarforschung 220
    RVK:
    RVK:
    Language: German
    Note: Literaturverz. S. 127 - 136 , Teilw. zugl.: Bremen, Univ., Diss., 1996
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  • 5
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The international multi-ship expedition ARCTIC'91 was able to collect a seismic transect between the Morris Jesup Rise and the Yermak Plateau. These conjugate plateau structures in the south-western part of the Eurasian Basin bound one of the slowest mid-oceanic spreading ridges in the world, the Gakkel Ridge. The seismic data reveal a sedimentary cover that is thin relative to the age of the oceanic crust at 83°N, 10°E and 85°N, 15°W. Close to the plateaus, thicker sequences are evident (Morris Jesup Rise, 500 m; Yermak Plateau, 1500 m). The seismic lines on the Morris Jesup Rise reveal only a thin sedimentary cover of 0.2 s TWT. In contrast, a layer with a thickness of almost 0.9 s TWT (1300 m) was found on the northernmost tip of the Yermak Plateau. The topography of the oceanic basement is very rough along the seismic lines, as could be expected at a slow spreading ridge. Depth variations of more than 1000 m are typical. Hydrosweep swath mapping provides the first detailed 3-D image from the Arctic mid-ocean ridge system at 87°N, 60°E and 84°N, 0°.
    Type of Medium: Electronic Resource
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  • 6
    Publication Date: 2021-03-29
    Description: report
    Keywords: 551.4 ; 551.22 ; 550 ; UKD 100 ; UHD 540 ; TOH 200 ; Expeditionsberichte {Regionale Ozeanologie, Indischer Ozean} ; Lange Wellen außer Gezeitenwellen {Dynamische Ozeanologie} ; Seismische Vorhersagen {Geophysik}
    Language: English
    Type: article , publishedVersion
    Format: 174 S.
    Format: application/pdf
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  • 7
    Publication Date: 2022-08-12
    Description: The Global Sea-level Observing System (GLOSS) was established by the Intergovernmental Oceanographic Commission (IOC) of the United Nations Educational, Scientific and Cultural Organization (UNESCO) in 1985 to provide oversight and coordination for global and regional sea-level networks in support of scien- tific research. The first GLOSS Implementation Plan (GIP) in 1990 established the GLOSS Core Network (GCN) of ~300 tide gauges distributed around the world, technical standards for GLOSS tide gauge stations, as well as the basic terms and obligations for Member States participating in GLOSS. The second GIP in 1997 expanded the GLOSS programme to include sub-networks focused on long historical records suitable for the detection of long-term sea- level trends and accelerations (GLOSS-LTT), a cali- bration network for satellite altimetry (GLOSS-ALT), and a network suitable for monitoring aspects of the global ocean circulation (GLOSS-OC). In addition, a strategy for integrating Global Positioning System (GPS) into monitoring of land levels at GLOSS tide gauges was developed. The focus of the GIP 2012 remains the GCN and the datasets that result from this network. The new plan calls for two significant upgrades to the GCN moti- vated by scientific and operational requirements: 1) all GCN stations are required to report data in near-real time, which will be tracked at a Sea-level Station Monitoring Facility. This will involve upgrades in power, data acquisition plat- forms, and communication packages; however, these upgrades are cost-effective in terms of the benefits that a real-time system will provide for ocean monitoring and improved station perfor- mance due to early detection of station malfunc- tions; 2) continuous measurements of the Global Navigation Satellite System (GNSS), in particular the U.S. Global Positioning System (GPS), the Russian GLONASS, or the newly established European GALILEO, or equivalent systems, in the vicinity of the tide gauge benchmark (TGBM) are required for all GCN stations. This upgrade will support satellite altimetry calibration and research efforts aimed at determining geocentric global sea-level rise rates as well as regional changes in sea level. Most relevant, vertical land movements can signifi- cantly alter the rates of sea-level rise expected from the sole climatic contributions of ocean ther- mal expansion and land-based ice melting, possi- bly magnifying the impacts of sea-level rise on the coast. In many cases, this requirement can be met by taking advantage of existing GNSS receivers maintained by other groups, as long as a precise geodetic tie to the GCN tide gauge can be made using, e.g. conventional levelling. The organization of the plan is as follows. An over- view of the GLOSS programme (chapter 1) and a brief summary of the uses of tide gauge data (chapter 2) are presented. The current status of the GLOSS programme is considered (chapter 3), followed by a discussion of the sea-level monitoring requirements raised by advisory groups and panels (chapter 4), as well as a self-assessment based on specific research and operational applications (chapter 5). These requirements are used to develop implementation goals for the GLOSS networks and data centres (chapter 6). Minor modifications are proposed for the administrative structure of GLOSS aimed at providing improved oversight of the imple- mentation plan (chapter 7). The success of the plan depends critically on the participation of Member States, whose obligations are summarized (chapter 8). The successful Training, Education and Mutual Assistance programmes that have been a corner stone of GLOSS will be continued to help meet implementation requirements (chapter 9). Additional technical and programmatic details are included in a set of appendices.
    Description: OpenASFA input
    Description: Published
    Description: Refereed
    Keywords: GLOSS ; Implementation plan ; ASFA_2015::S::Sea level
    Repository Name: AquaDocs
    Type: Report
    Format: 44pp.
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  • 8
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: ANT-IX/4; AWI_Paleo; CT; DATE/TIME; LATITUDE; LONGITUDE; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS18; PS18/4-track; Swath-mapping system Atlas Hydrosweep DS-1; Underway cruise track measurements; Uniform resource locator/link to raw data file
    Type: Dataset
    Format: text/tab-separated-values, 876 data points
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  • 9
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-05-12
    Description: From data collected by RV Polarstern, and additional echosoundings provided by national hydrographic offices, research institutions and the International Hydrographic Organization (IHO) Digital Bathymetric Data Center, the 1:1,000,000 Bathymetric Chart of the Weddell Sea (AWl BCWS) series has been developed. The heterogeneity of bathymetric data and the lack of observations within ice-covered areas required the incorporation of supplementary geophysical and geographical information. A semi-automatic procedure was developed for terrain modeling and contouring. In coastal regions, adjacent sub-glacial information was included in order to model the bathymetry of the transition zone along the Antarctic ice edge. Six sheets of the AWl BCWS series in the scale of 1:1,000,000 covering the southern Weddell Sea from 66°S to 78°S and from 68°W to 0°E were recently completed and included in the 1997 GEneral Bathymetric Chart of the Oceans (GEBCO) Digital Atlas CD-ROM (http://www.gebco.net). On the basis of these six 1:1,000,000 AWl BCWS sheets, a generalized 1:3,000,000-scale bathymetric chart was compiled for the entire southern Weddell Sea.
    Keywords: Area/locality; LATITUDE; Latitude 2; LONGITUDE; Longitude 2; ORDINAL NUMBER; Scale; Status; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 69 data points
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  • 10
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    PANGAEA
    In:  Supplement to: Gingele, Franz; Kuhn, Gerhard; Maus, Bastian; Melles, Martin; Schöne, Tilo (1997): Holocene ice retreat from the Lazarev Sea shelf, East Antarctica. Continental Shelf Research, 17(2), 137-163, https://doi.org/10.1016/S0278-4343(96)00026-X
    Publication Date: 2023-06-27
    Description: Distinct facies types, classified in radiocarbon-dated sediments from the shelf of the Lazarev Sea, East Antarctica, reveal a detailed history of processes that have controlled sedimentation during the deglaciation over the last 10,000 yr. The ice retreat on this part of the Antarctic shelf started 9500 yr BP, marked by the deposition of laminated sediments, deposited from a floating ice shelf. These laminites, which occur on top of diamictons laid down from a grounded ice sheet, are the basal sediments of the postglacial sequence. The intensity of the Antarctic Coastal Current (ACC), directed by shelf morphology, controlled sedimentation of the postglacial facies. A residual glaciomarine sediment with the fine fraction winnowed by strong currents developed from 9000-8000 yr BP in the western part of the investigation area and from 9000-5000 yr BP in the eastern part, closer to the prominent 'Fenno Deep' trough. Current velocities apparently decreased between 8000 and 2000 yr BP due to a deflection of the ACC by advancing ice tongues to the east of the investigation area during the 'Hypsithermal'. This led to a deposition of fine-grained sediments, and clay mineralogy suggests a continental source, possibly near the grounding line of the Nivl Ice Shelf, rather than a winnowing of sediments near the shelf break or advection from deeper water. Current velocities intensified after 2000 yr BP, removed fine material from these sediments and led to a relict sediment, consisting of coarse bryozoan and molluscan debris.
    Keywords: ANT-IX/3; ANT-X/2; AWI_Paleo; Giant box corer; GKG; Gravity corer (Kiel type); Lazarev Sea; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS18; PS18/175; PS18/208; PS18/209; PS20; PS20/219; PS20/221; PS20/222; PS2028-1; PS2028-2; PS2028-4; PS2057-2; PS2058-1; PS2058-2; PS2226-3; PS2227-1; PS2228-2; SL; Weddell Sea
    Type: Dataset
    Format: application/zip, 21 datasets
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