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Geoid Determination Based on a Combination of Terrestrial and Airborne Gravity Data in South Korea

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Geoid Determination Based on a Combination of Terrestrial and Airborne Gravity Data in South Korea Geoid Determination based on a Combination of Terrestrial and Airborne Gravity Data in South Korea DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Hyo Jin Yang Graduate Program in Geodetic Science and Surveying The Ohio State University 2014 Dissertation Committee: Professor Christopher Jekeli, Advisor Professor Michael Bevis Professor Ralph R.B. von Frese Copyright by Hyo Jin Yang 2014 ABSTRACT The regional gravimetric geoid model for South Korea is developed by using heterogeneous data such as gravimetric measurements, a global geopotential model, and a high resolution digital topographic model. A highly accurate gravimetric geoid model, which is a basis to support the construction of the efficient and less costly height system with GPS, requires many gravimetric observations and these are acquired by several kinds of sensors or on platforms. Especially airborne gravimetry has been widely employed to measure the earth’s gravity field in last three decades, as well as the traditional measurements on the earth’s physical surface. Therefore, it is necessary to understand the characters of each gravimetric measurement, such as the measurement surface and involved topography, and also to integrate these to a unified gravimetric data base which refers to the same gravitational field. This dissertation illustrates the methods for combining two types of available gravity data for South Korea, one is terrestrial data obtained on the earth’s surface and another is airborne data measured at altitude, and shows an accessible accuracy of the geoid model based on these data. It is found that there exists some bias between terrestrial and airborne gravimetric data probably due to their different properties, and the bias is significantly reduced by the terrain effects determined by the Bouguer reduction. Therefore, the gravimetric data should be merged to a unified data base in terms of the Bouguer gravity anomaly. The reductions are the important roles not only to combine gravimetric data, but also to satisfy the boundary conditions of the Stokes’s integral. The Stokes’s integral is applied to the unified gravimetric data set in order to model the geoid undulation for South Korea. ii Also the systematic effects on the fundamental equation of physical geodesy are numerically demonstrated on the gravity anomaly and geoid undulation. These are shown to be negligible. In addition, the limitations of the Stokes’s integral caused by truncation of the integration area and discontinuity of data are reduced by the empirical application of the Stokes’s kernel modification and the Remove-Compute-Restore technique. The demonstration of accuracy of the developed geoid model, which is compared to GPS/leveling, shows the model based on the gravity anomaly with respect to the terrain effects have better accuracy than the model based on the free-air gravity anomaly. The achievement on the precision of geoid undulation, computed on a 2 arcmin grid, is 5.6 cm in standard deviation. This model is based on the airborne-only gravity data considering not only the terrain effects but also the downward continuation. The bias in the gravimetric geoid of about 15.5 cm, determined from the comparison with the GPS/leveling data, agrees with previously determined values. iii DEDICATION To My Family iv ACKNOWLEDGMENTS First, I would like to specially thank my advisor, Dr. Christopher Jekeli, for his advice, guidance, encouragement, and support during my Ph.D in The Ohio State University. He is the best advisor and instructor in my life. I wish to thank Dr. Ralph von Frese, Dr. C.K. Shum and Dr. Michael Bevis for their valuable comments and suggestions as my committee members and class instructor. And I would like to thank Dr. Jay Hyoun Kwon in Department of Geoinformatics, The University of Seoul, Korea for his advice and support. Thank mom, dad, and my sisters (and Jihye Park) and brother for all support, faith, and love. v VITA February 2005 ...................................................................... B.S. , The University of Seoul 2007...................................................................................... M.S. , The University of Seoul 2010 ................................................................................ M.S. , The Ohio State University 2007 to present .............................................. Graduate Research Associate, Geodetic Science Program, School of Earth Science, The Ohio State University Publications Jekeli C, Yang HJ, Kwon JH (2009a) Evaluation of EGM08 – Globally and Locally in South Korea. Newtons Bulletin 4:38–49. Jekeli C, Yang HJ, Kwon JH (2009b) Using gravity and topography-implied anomalies to assess data requirements for precise geoid computation. Journal of Geodesy 83:1193–1202. doi: 10.1007/s00190-009-0337-y Jekeli C, Yang HJ, Kwon JH (2012) The offset of the South Korean vertical datum from a global geoid. KSCE Journal of Civil Engineering 16:816–821. doi: 10.1007/s12205-012-1320-3 Jekeli C, Yang HJ, Ahlgren K (2013) Using isostatic gravity anomalies from spherical harmonic models and elastic plate compensation to interpret the lithosphere of the Bolivian Andes. GEOPHYSICS 78:G41–G53. doi: 10.1190/GEO2012-0378.1 Fields of Study Major Field: Geodetic Science and Surveying vi TABLE OF CONTENTS ABSTRACT .........................................................................................................................ii DEDICATION .................................................................................................................... iv ACKNOWLEDGMENTS ................................................................................................... v VITA ................................................................................................................................... vi TABLE OF CONTENTS ................................................................................................... vii LIST OF TABLES .............................................................................................................. xi LIST OF FIGURES .......................................................................................................... xiv ACRONYMS ................................................................................................................... xvii CHAPTER 1 INTRODUCTION ..................................................................................... 1 1.1 Background .......................................................................................................... 1 1.2 Statement of problem ........................................................................................... 8 1.3 Objectives and chapter description .................................................................... 11 CHAPTER 2 THEORETICAL BACKGROUND OF GEOID DETERMINATION .. 14 2.1 Geodetic Boundary Value Problem and Bruns’ equation .................................. 15 2.2 Determination of geoid undulation .................................................................... 18 vii 2.2.1 Gravity anomaly.......................................................................................... 18 2.2.2 Stokes’s integral .......................................................................................... 20 2.3 Systematic effects ............................................................................................... 23 2.3.1 Atmospheric correction ............................................................................... 23 2.3.2 Directional Derivative error ........................................................................ 24 2.3.3 Linear approximation error ......................................................................... 25 2.3.4 Spherical approximation error .................................................................... 26 2.3.5 Ellipsoidal correction .................................................................................. 28 2.4 Reductions .......................................................................................................... 30 2.4.1 Topographic effects .................................................................................... 30 2.4.2 Indirect effect .............................................................................................. 38 2.4.3 Analytic continuation .................................................................................. 40 2.5 Remove-Compute-Restore principle and chapter summary .............................. 45 CHAPTER 3 CONSTRUCTION OF UNIFIED GRAVITY ANOMALY DATASET 51 3.1 Datasets for South Korea.................................................................................... 51 3.1.1 Terrestrial gravity measurement ................................................................. 54 3.1.2 Airborne gravity measurement ................................................................... 57 3.1.3 Consistency between gravimetric measurements ....................................... 59 3.1.4 GPS/leveling data........................................................................................ 62 viii 3.2 Global Geopotential Models (GGMs) ................................................................ 64 3.2.1 Earth Gravitational Models 1996 and 2008 ................................................ 65 3.2.2 Global Geopotential Models based on GOCE ............................................ 68 3.2.3 Analysis of Global Geopotential
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