Journals / Harita Dergisi / 2007 / Cilt: 73 - Sayı: 18

High-degree geopotential model tailored to Egypt

Pages
187–192
DOI
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AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

The results show that the tailored geopotential models give better residual gravity anomalies.

📌 3 Key Takeaways

🎯
Objective & Hypothesis:The quality of the reference geopotential model used in the framework of the removerestore technique greatly affects the accuracy of the computed geoid.
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Key Findings & Data:The aim of this investigation is to have a smoothed gravity field so that it is unbiased and has significantly reduced variance by using a high-degree tailored geopotential model.
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Conclusion & Impact:The results show that the tailored geopotential models give better residual gravity anomalies.
🔬Design:Modeling & Simulation
📍Scope:2004 Verileri
⚙️Variables:Domain Parameters

Abstract

The quality of the reference geopotential model used in the framework of the removerestore technique greatly affects the accuracy of the computed geoid. None of the existing geopotential models fit the Egyptian gravity field to the desired extent. The aim of this investigation is to have a smoothed gravity field so that it is unbiased and has significantly reduced variance by using a high-degree tailored geopotential model. The window technique has been applied to get rid of the double consideration of the topographic-isostatic masses within the data window. The high-degree tailored reference model has been created by merging the available gravity anomalies in the area of investigation with the EGM96 global gravitational data set. The merged global field has been used to estimate the harmonic coefficients of the tailored reference model by FFT technique using an iteration process to enhance the accuracy of the obtained harmonic coefficients (Abd- Elmotaal, 2004). Three different tailored geopotential models have been created by maintaining the lower harmonics till degree 20, 36 and 72 to their values as of EGM96 model. The results show that the tailored geopotential models give better residual gravity anomalies. The variance has dropped to its one third.

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Cite This Article

ABD-ELMOTAAL, H. A. (2007). High-degree geopotential model tailored to Egypt. Harita Dergisi, Cilt: 73 - Sayı: 18, 187–192. https://ajindex.com/articles/193296

References (2)

  1. Abd-Elmotaal, H. (2004) An Efficient Technique for Harmonic Analysis on a Spheroid (Ellipsoid and Sphere), Österreichische Zeitschrift fiir Vermes-sung & Geoinformation, 3+4, 126 135. Abd-Elmotaal, H. (1999) The EGHA99 Digital Height Models for Egypt, Proceedings of the 1st Minia International Conference for Advanced Trends in Engineering, Minia, Egypt, March 14-16, 1999,1,205 211. Abd-Elmotaal, H. and KOhtreiber, N. (2003) Geoid Determination Using Adapted Reference Field, Seismic Moho Depths and Variable Density Contrast, Journal of Geodesy, 77, 77 85. Colombo, O. (1981) Numerical Methods for Harmonic Analysis on the Sphere, Department of Geodetic Science, The Ohio State University, Columbus, Ohio, 310. Heiskanen, W.A., and Moritz, H. (1967)
  2. Physical Geodesy. Freeman, San Francisco. Wenzel, H.G. (1998) Ultra High Degree Geopotential Models GPM98A, B and C to Degree 1800, URL:http://www.gik.uni-karlsruhe. de/~wenzel/gpm98abc/gpm98abc.htm