| Foreword | p. x |
| How to Climb the Gravity Wall | p. 1 |
| Precise Orbit Determination and Gravity Field Modelling | |
| Strategies for Precise Orbit Determination of Low Earth Orbiters Using the GPS | p. 17 |
| Aiming at a 1-cm Orbit for Low Earth Orbiters: Reduced-Dynamic and Kinematic Precise Orbit Determination | p. 27 |
| Space-Wise, Time-Wise, Torus and Rosborough Representations in Gravity Field Modelling | p. 37 |
| Gravity Field Recovery From GRACE: Unique Aspects of the High Precision Inter-Satellite Data and Analysis Methods | p. 47 |
| Global Gravity Field Recovery Using Solely GPS Tracking and Accelerometer Data from CHAMP | |
| The Processing of Band-Limited Measurements: Filtering Techniques in the Least Squares Context and in the Presence of Data Gaps | p. 67 |
| Solid Earth Physics | |
| Long Wavelength Sea Level and Solid Surface Perturbations Driven by Polar Ice Mass Variations: Fingerprinting Greenland and Antarctic Ice Sheet Flux | p. 81 |
| Benefits From GOCE within Solid Earth Geophysics | p. 95 |
| The Potential of GOCE in Constraining the Structure of the Crust and Lithosphere from Post-Glacial Rebound | p. 105 |
| Deep and Shallow Solid-Earth Structures Reconstructed with Sequential Integrated Inversion (SII) of Seismic and Gravity Data | p. 115 |
| Present-Day Sea Level Change: Observations and Causes | p. 131 |
| Ocean Circulation | |
| Global Ocean Data Assimilation and Geoid Measurements | p. 147 |
| Resolution Needed for an Adequate Determination of the Mean Ocean Circulation from Altimetry and an Improved Geoid | p. 163 |
| Error Characteristics Estimated from CHAMP, GRACE and GOCE Derived Geoids and from Satellite Altimetry Derived Mean Dynamic Topography | p. 179 |
| Estimating the High-Resolution Mean Sea-Surface Velocity Field by Combined Use of Altimeter and Drifter Data for Geoid Model Improvement | p. 195 |
| Combined Use of Altimetry and In Situ Gravity Data for Coastal Dynamics Studies | p. 205 |
| Feasibility, and Contribution to Ocean Circulation Studies, of Ocean Bottom Pressure Determination | p. 217 |
| Impact of Geoid Improvement on Ocean Mass and Heat Transport Estimates | p. 225 |
| How Operational Oceanography can Benefit from Dynamic Topography Estimates as Derived From Altimetry and Improved Geoid | p. 239 |
| Geodesy | |
| Remarks on the Role of Height Datum in Altimetry-Gravimetry Boundary-Value Problems | p. 253 |
| Ocean Tides In GRACE Monthly Averaged Gravity Fields | p. 261 |
| Tidal Models in a New Era of Satellite Gravimetry | p. 271 |
| The Elusive Stationary Geoid | p. 283 |
| Geodetic Methods for Calibration of GRACE and GOCE | p. 293 |
| Sea Level | |
| Benefits of GRACE and GOCE to Sea Level Studies | p. 307 |
| What Might GRACE Contribute to Studies of Post Glacial Reboud? | p. 319 |
| Measuring the Distribution of Ocean Mass Using GRACE | p. 331 |
| Monitoring Changes in Continental Water Storage with GRACE | p. 345 |
| Future Concepts | |
| Attitude and Drag Control: An Application to the GOCE Satellite | p. 357 |
| On Superconductive Gravity Gradiometry in Space | p. 367 |
| Satellite-Satellite Laser Links for Future Gravity Missions | p. 377 |
| Possible Future Use of Laser Gravity Gradiometers | p. 385 |
| Microscope Instrument Development, Lessons for GOCE | p. 393 |
| Needs and Tools for Future Gravity Measuring Missions | p. 409 |
| Closing Session | |
| Goce: Esa's First Earth Explorer Core Mission | p. 419 |
| Earth Gravity Field From Space--From Sensors to Earth Sciences: Closing Remarks | p. 433 |
| Author Index | p. 443 |
| List of Participants | p. 445 |
| Table of Contents provided by Ingram. All Rights Reserved. |