Evaluation of EGM96 and EGM08 based on GPS/Levelling Heights in Egypt

IF 0.3 Q4 REMOTE SENSING South African Journal of Geomatics Pub Date : 2023-02-15 DOI:10.4314/sajg.v12i1.3
Khaled Mahmoud Abdel Aziz, Karim Samir Rashwan, Nasr Saba
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引用次数: 1

Abstract

The heights determined by  Global Positioning System (GPS) refer to the ellipsoid called the World Geodetic System 1984 (WGS84).  Global Geopotential Models (GGMs) that are available on GNSS commercial software are generally used to transform  ellipsoidal heights to orthometric heights. In this study, the geoid heights of GPS/Levelling were computed to evaluate the accuracy of the geoid heights obtained from two GGMs, namely, the Earth Gravitational Model 96 (EGM96) and the Earth Gravitational Model 08 (EGM08). Seventeen (17) GPS/Levelling stations of the High Accuracy Reference Network (HARN) over Egypt were used for this purpose. The standard deviations for the differences between the geoid heights obtained through GPS/Levelling and those obtained from EGM96 and EGM08 were determined as  ± 1.212 m and ± 0.543 m, respectively. This research confirms that the geoid heights obtained from EGM08 are closer to the geoid heights determined using GPS/Levelling over Egypt.
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基于GPS/水准高度的埃及EGM96和EGM08评价
全球定位系统(GPS)确定的高度是指被称为1984年世界大地测量系统(WGS84)的椭球体。全球导航卫星系统商业软件上提供的全球地球位势模型(GGM)通常用于将椭球高度转换为正交高度。在本研究中,计算了GPS/水准测量的大地水准面高度,以评估从两个GGM(即地球引力模型96(EGM96)和地球引力模型08(EGM08))获得的大地水准面的精度。埃及上空高精度参考网的十七(17)个全球定位系统/水准测量站用于此目的。通过GPS/水准测量获得的大地水准面高度与通过EGM96和EGM08获得的大地水平面高度之差的标准偏差分别为±1.212m和±0.543m。这项研究证实,从EGM08获得的大地水准面高度更接近埃及上空使用GPS/Leveling确定的大地水准面的高度。
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