Assessment of Geoidal Undulation (N) Values Computed with Reference to Different Earth Gravity Models

Benjamin John Bulangas, A. Mohammed, M. Ismaila
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引用次数: 1

Abstract

This research entails the determination of the variations in global geoid undulation with reference to different Earth Gravity Models (EGMs). Geoidal undulation values of 22 points selected within the study area were determined from GPS derived data on differential mode. The undulation values were computed with reference to three different earth gravity models (EGM84, EGM96 and EGM2008) which use geopotential coefficients and spherical harmonic analysis. The results obtained were plotted and the configuration of the local geoid was obtained with respect to each gravity model. It was observed that structural development in the school (study area) since its inception in 1981 has forced some significant changes in the mass distribution in the school and consequently changes in gravity values which in turn changes the undulation values (which depends on gravity) from point to point. It was also observed that there was correlation between the local geoid determined and the nature of the topography. Areas with higher ellipsoidal or orthometric heights experience greater separation between the geoid and the ellipsoid.
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参考不同地球重力模型计算大地面波动(N)值的评估
这项研究需要确定参考不同地球重力模型(egm)的全球大地水准面波动的变化。利用差分模式下的GPS数据,确定了研究区内选取的22个点的大地水准面波动值。参考EGM84、EGM96和EGM2008三种不同的地球引力模型,分别采用位势系数和球谐分析计算了其波动值。对所得结果进行了绘图,并得到了各重力模型的局部大地水准面构型。据观察,自1981年建校以来,学校(研究区域)的结构发展迫使学校的质量分布发生了一些重大变化,从而改变了重力值,从而改变了点与点之间的波动值(这取决于重力)。还观察到,确定的局部大地水准面与地形性质之间存在相关性。椭球面高度或正交高度较高的区域在大地水准面和椭球面之间有较大的分离。
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