Gravity, Geoid and Geodynamics 2000: GGG2000 IAG International Symposium Banff, Alberta, Canada July 31 August 4, 2000 [Paperback]

Time Variable Gravity: An Emerging Frontier in Interdisciplinary Geodesy.- Earth Physics and Global Glacial Isostasy: from Paleo-Geodesy to Space-Geodesy.- Global Unification of Height Systems and GOCE.- A Discussion of Fundamental Constants in View of Geodetic Reference Systems.- A Study of the Transfer of the ITRF Datum to a GPS Network in Antarctica.- Establishing Global Reference Frames. Nonlinear, Temporal, Geophysical and Stochastic Aspects.- Aliasing Error Modeling in Single-Input Single-Output Linear Estimation Systems.- Integrating Heterogeneous Data Sets with Partial Inconsistences.- Optimization of Computations in Spherical Geopotential Field Applications.- TcLight: a New Technique for Fast RTC Computation.- A Fast, Spatial Domain Technique for Terrain Corrections in Gravity Field Modeling.- Some Considerations on Fuzzy Least-Squares.- A Wavelet Solution to 1D Non-Stationary Collocation With an Extension to 2D Case.- A Wavelet Based Gravity Model with an Application to the Evaluation of Stokes Integral.- Satellite Gravity Anomaly Recovery Using Multigrid Methods.- Inverting Land Uplift near Vatnaj?kull, Iceland, in Terms of Lithosphere Thickness and Viscosity Stratification.- Error Analysis of the Gravity Recovery and Climate Experiment (GRACE) Mission.- GOCE Gravity Field Recovery Using Massive Parallel Computing.- Regularization for the Gravity Field Recovery from GOCE Observations.- Local Geoid Determination with in situ Geopotential Data Obtained from Satellite-to-Satellite Tracking.- Energy Relations for the Motion of two Satellites within the Gravity Field of the Earth.- Dynamic Satellite Geodesy on the Torus: Block-Diagonality from a Semi-Analytical Approach.- Evaluation of Temporal Variations on the Gravity Field Caused by Geophysical Fluids andTheir Possible Detection by GRACE.- GRIM5-C1: Combination Solution of the Global Gravity Field to Degree and Order 120.- High Resolution Gravity Field Modeling with Full Variance-Covariance Matrices.- Gravls¬