利沃夫地区几何大地水准面stha模型的构建

F. Zablotskyi, B. Dzhuman
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引用次数: 1

摘要

如今,乌克兰需要对其高空系统进行现代化改造,这就需要将其纳入欧洲垂直参考系统EVRS。在这方面,还需要在我国境内建立一个与欧洲大地水准面EGG2015模型很好吻合的区域大地水准面模型。为了获得最优模型,需要同时使用重力和几何数据。在这种情况下,这个模型被称为重力几何模型。这种方法既用于建立欧洲大地水准面模型,也用于在不同欧洲国家的领土上建立大地水准面模型。的目标。本文旨在建立利沃夫地区大地水准面区域几何stha模型,并对其精度进行评价。未来计划在同一地区建立大地水准面重力stha模型,并对结果进行比较。方法。为了在Lviv区域上建立大地水准面几何stha模型,我们使用gnss在SGN的I、II和III类点上观测得到的几何大地水准面高度。静态模式下GNSS水准测量所得大地高程的均方根误差不超过15 mm,利用205个计算出的大地水准面高程值建立大地水准面模型。8个值不参与模型的构建,因为它们是用于独立评估模型精度的。结果。引入正则化参数,得到了“移除-计算-恢复”过程中大地水准面区域模型。所得模型的均方根误差(RMS error)在构建模型所用数据的基础上计算为12 mm,在其他独立数据上计算为25 mm。具有科学新颖性和现实意义。首次利用stha函数建立区域大地水准面模型。计算了Lviv地区大地水准面几何模型,并根据相关和独立数据对模型的精度进行了估计。所得模型的均方根误差约为2 cm,与gnss测量精度相当。得到的模型可以作为Lviv地区的变换场。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Construction of STHA-model of geometric geoid on the Lviv region area
Nowadays there is a need to modernize the high system of Ukraine, which requires its integration in the European Vertical Reference System EVRS. In this regard there is also a need to build a regional model of the geoid on the territory of our country, which would be well consistent with the model of the European geoid EGG2015. To obtain the optimal model, it is necessary to use both gravimetric and geometric data. In this case, the model is called gravimetric-geometric. This approach is used both when building a model of the European geoid and when building geoid models on the territory of different European countries. Aim. The purpose of this work is to build a regional geometric STHA-model of the geoid on the Lviv region area and assess its accuracy. In the future it is planned to build a gravimetric STHA-model of the geoid in the same area and compare the results. Methods. To build a geometric STHA-model of the geoid on the Lviv region area, the heights of the geometric geoid, obtained from GNSS-observations at the points of SGN of I, II and III classes, were used. RMS error of determination of geodetic heights , obtained from GNSS leveling in static mode, did not exceed 15 mm. 205 values of the calculated heights of the geoid were used to build the geoid model. 8 values were not involved in the construction of the model, because they were used for an independent assessment of model accuracy. Results. The regional model of geoid within the “Remove–Compute–Restore” procedure with introduction of regularization parameter is obteined. RMS error of the obtained model, calculated on the basis of the data used in its construction, is 12 mm, and on other independent data is 25 mm. Scientific novelty and practical significance. For the first time STHA-functions were tested to build a regional geoid model. The geometric model of the geoid on the Lviv region are is calculated and the accuracy of the obtained model is estimated on the basis of dependent and independent data. The RMS error of the obtained model was about 2 cm, which corresponds to the accuracy of GNSS-measurements. The obtained model can be used as a transformation field on the Lviv region area.
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