IAG 150 Years pp 233-239 | Cite as
Regional Gravity Field Modeling by Radially Optimized Point Masses: Case Studies with Synthetic Data
- 1.8k Downloads
Abstract
A two-step point mass method with free depths is presented for regional gravity field modeling based on the remove-compute-restore (RCR) technique. Three numerical test cases were studied using synthetic data with different noise levels. The point masses are searched one by one in the first step with a simultaneous determination of the depth and magnitude by the Quasi-Newton algorithm (L-BFGS-B). In the second step, the magnitudes of all searched point masses are readjusted with known positions by solving a linear least-squares problem. Tikhonov regularization with an identity regularization matrix is employed if ill-posedness exists. One empirical and two heuristic methods for choosing proper regularization parameters are compared. In addition, the solutions computed from standard and regularized least-squares collocation are presented as references.
Keywords
Free depths Least-squares collocation Point mass method Regional gravity field modeling Tikhonov regularizationNotes
Acknowledgements
Three anonymous reviewers are acknowledged for their valuable comments which improved the original manuscript. The first author is financially supported by China Scholarship Council (CSC) for his PhD study in Germany.
References
- Ameti P (2006) Downward continuation of Geopotential in Switzerland. PhD Thesis, TU Darmstadt, Darmstadt, GermanyGoogle Scholar
- Antunes C, Pail R, Catalão J (2003) Point mass method applied to the regional gravimetric determination of the geoid. Stud Geophys Geod 47:495–509CrossRefGoogle Scholar
- Barthelmes F (1986) Untersuchungen zur approximation des äußeren Schwerefeldes der Erde durch Punktmassen mit optimierten Positionen. Report Nr. 92, Veröffentlichungen des Zentralinstitut Physik der Erde, Potsdam, GermanyGoogle Scholar
- Bentel K, Schmidt M, Gerlach C (2013) Different radial basis functions and their applicability for regional gravity field representation on the sphere. GEM Int J Geomath 4:67–96CrossRefGoogle Scholar
- Bjerhammar A (1986) Megatrend solutions in physical geodesy. NOAA Technical Report No. 116 NGS 34, National Oceanic and Atmospheric Administration, USAGoogle Scholar
- Bouman J (1998) Quality of regularization method. DEOS Report Nr. 98.2, Delft Institute for Earth-Orient Space Research, Delft University of Technology, Delft, NetherlandsGoogle Scholar
- Bowin C (1983) Depth of principal mass anomalies contributing to the earth’s geoidal undulations and gravity anonalies. Mar Geod 7:61–100CrossRefGoogle Scholar
- Byrd RH, Lu P, Nocedal J, Zhu C (1995) A limited memory algorithm for bound constrained optimization. SIAM J Sci Comput 16:1190–1208CrossRefGoogle Scholar
- Claessens SJ, Featherstone WE, Barthelmes F (2001) Experiences with point-mass gravity field modeling in the Perth Region, Western Australia. Geomet Res Aust 75:53–86Google Scholar
- Eicker A (2008) Gravity field refinement by radial basis functions from in-situ satellite data. PhD Thesis, University of Bonn, Bonn, GermanyGoogle Scholar
- Klees R, Tenzer R, Prutkin I, Wittwer T (2008) A data-driven approach to local gravity field modeling using spherical radial basis functions. J Geod 82:457–471CrossRefGoogle Scholar
- Koch K-R, Kusche J (2002) Regularization of geopotential determination from satellite data by variance components. J Geod 76:259–268CrossRefGoogle Scholar
- Kusche J, Klees R (2002) Regularization of gravity field estimation from satellite gravity gradients. J Geod 76:359–368CrossRefGoogle Scholar
- Lehmann R (1993) The method of free-positioned point masses-geoid studies on the Gulf of Bothnia. Bull Géod 67:31–40CrossRefGoogle Scholar
- Lin M, Denker H, Müller J (2014) Regional gravity field modeling using free-positioned point masses. Stud Geophys Geod. doi: 10.1007/s11200-013-1145-7 Google Scholar
- Marchenko AN, Tartachynska ZR (2003) Gravity anomalies in the Black sea area derived from the inversion of GEOSAT, TOPEX/POSEIDON and ERS-2 altimetry. Bull Geod Sci Affini LXII:50–62Google Scholar
- Marchenko AN, Barthelmes F, Mayer U, Schwintzer P (2001) Regional geoid determination: an application to airborne gravity data in the Skagerrak. Scientific Technical Report No. 01/07, GFZ, Potsdam, GermanyGoogle Scholar
- Mayer-Gürr T, Rieser D, Höck E, Brockmann JM, Schuh W, Krasbutter I, Kusche J, Maier A, Krauss S, Hausleitner W, Baur O, Jäggi A, Meyer U, Prange L, Pail R, Fecher T, Gruber T (2012) The new combined satellite only model GOCO03s. International Symposium on Gravity, Geoid and Height Systems, Venice, Italy, October 9–12 (oral presentation)Google Scholar
- Moritz H (1980) Advanced physical geodesy. Herbert Wichman, KarlsruheGoogle Scholar
- Nocedal J, Wright SJ (1999) Numerical optimization. Springer, New YorkCrossRefGoogle Scholar
- Pavlis NK, Holmes SA, Kenyon SC, Factor JK (2012) The development and evaluation of the earth gravitational model 2008 (EGM2008). J Geophys Res 117:B04406. doi: 10.1029/2011JB008916 CrossRefGoogle Scholar
- Schmidt M, Fengler M, Mayer-Guerr T, Eicker A, Kusche J, Sanchez L, Han S (2007) Regional gravity field modeling in terms of spherical base functions. J Geod 81:17–38CrossRefGoogle Scholar
- Tenzer R, Klees R (2008) The choice of the spherical radial basis functions in local gravity field modeling. Stud Geophys Geod 52:287–304CrossRefGoogle Scholar
- Tikhonov AN (1963) Solution of incorrectly formulated problems and the regularization method. Soviet Math Dokl 4:1035–1038Google Scholar
- Tscherning CC, Rapp RH (1974) Closed covariance expressions for gravity anomalies, geoid undulations and deflections of the vertical implied by anomaly degree variance models. OSU Report 208, Department of Geodetic Science and Surveying, Ohio State University, Columbus, Ohio, USAGoogle Scholar
- Zhu C, Byrd RH, Lu P, Nocedal J (1994) LBFGS-B: fortran subroutines for large-scale bound constrained optimization. Report NAM-11, EECS Department, Northwestern University, Evanston, IL, USAGoogle Scholar