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On determining orthometric heights from a corrector surface model based on leveling observations, GNSS, and a geoid model

机译:根据基于水准观测,GNSS和大地水准面模型的校正器表面模型确定正高

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Leveling is a traditional geodetic surveying technique that has been used to realize a vertical datum. However, this technique is time consuming and prone to accumulate errors, where it relies on starting from one station with a known orthometric height. Establishing ortho-metric heights using Global Navigation Satellite Systems (GNSS) and a geoid model has been suggested [14], but this approach may involve less precisions than the direct measurements from leveling. In this study, an experimental study is presented to adjust the highly accurate leveling observations along with orthometric heights derived from GNSS observations and a geoid model. For the geoid model, the National Geodetic Survey's gravimetric geoid model (TxGE0ID16B) and hybrid geoid model (GE0ID12B) were applied. Uncertainties in the leveled height differences, GNSS derived heights, and the geoid models were modeled, and a combined adjustment was implemented to construct the optimal combination of orthometric, ellipsoidal, and geoid height at each mark. As a result, the discrepancy from the published orthometric heights and the CSM (Corrector Surface Model) based adjusted ortho-metric heights with GE0ID12B showed a mean and RMS of -8.5 mm and 16.6 mm, respectively, while TxGE0ID16B had a mean and RMS of 28.9 mm and 34.6 mm, respectively. It should be emphasized that this approach was not influenced by the geodetic distribution of the stations where the correlation coefficients between the distance from the center of the surveying network and the discrepancy from the published heights using TxGE0ID16B and GE0ID12B are 0.03 and 0.36, respectively.
机译:调平是一种传统的大地测量技术,已用于实现垂直基准。但是,该技术非常耗时并且容易累积错误,在这种情况下,它依赖于从已知正交高度的一个测站开始。有人建议使用全球导航卫星系统(GNSS)和大地水准面模型建立正交高程[14],但是这种方法所涉及的精度可能比来自水准测量的直接测量精度低。在这项研究中,进行了一项实验研究,以调整高精度的水准观测值以及从GNSS观测值和大地水准面模型得出的正高。对于大地水准面模型,应用了美国大地测量局的重力大地水准面模型(TxGE0ID16B)和混合大地水准面模型(GE0ID12B)。对水平高度差,GNSS导出的高度和大地水准面模型的不确定性进行建模,并进行组合调整以构造每个标记处的正高,椭球形和大地水准面高度的最佳组合。结果,与发布的正高和与GE0ID12B的基于CSM(校正表面模型)的已调整正高的差异分别显示出-8.5 mm和RMS的均方根值和16.6 mm,而TxGE0ID16B的均值和RMS均方根值分别为28.9毫米和34.6毫米。应当强调的是,该方法不受测站的大地测量分布的影响,测站的中心距与使用TxGE0ID16B和GE0ID12B发布的高度之间的相关系数分别为0.03和0.36。

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