On quality of NKG2015 geoid model over the Nordic countries

IF 0.9 Q4 REMOTE SENSING
M. Eshagh, Jenny Berntsson
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引用次数: 4

Abstract

Abstract The NKG2015 geoid model covers the Nordic and Baltic countries and has been computed based on the least-squares modification of Stokes’ formula with additive corrections method. New and precise terrestrial, airborne and shipborne gravimetric measurements, the recent global gravity model of the gravity field and steady-state ocean circulation explorer (GOCE) and detailed digital terrain models over each territory have been used for computing this new geoid model. Some estimates for the error of this model have been roughly presented by comparing it with the global navigation satellite system (GNSS) data over each country. In this paper, our goal is to have a closer look at the relative error of this model by performing some statistical tests and finding the proper corrective surface for absorbing the systematic errors over each country. Our main assumption is realisticity of the errors of GNSS/levelling data and we will investigate its consequences in estimating the error of the geoid model. Our results show that the 4-parameter corrective surface is suitable for modelling the systematic trends of the differences between the gravimetric and GNSS geoid heights in Sweden, Denmark and Finland, but a filtered discrepancies by a confidence interval of 95% should be used for Sweden. A 7-aparameter model is suitable for the filtered discrepancies with the confidence interval of 95% in Norway. Based on the selected corrective surface and our newly developed regional iterative variance estimator, the confidence interval for the error of NKG2015 geoid model in Sweden, Denmark and Norway yielded 0-6.5 mm, 1.8-5.2 mm, 14.8-17.7 mm, respectively with a confidence level of 95%. We could not estimate the geoid error in Finland because the given error of the GNSS/levelling heights is significantly larger than the size of residuals. Based on the selected corrective surfaces and our presented local variance estimator, the average error of geoid becomes 3.6, 2.4, 8.8 and 5.8 mm with a confidence interval of 68%, respectively, over Sweden, Denmark, Norway and Finland.
北欧国家NKG2015大地水准面模型质量研究
NKG2015大地水准面模型覆盖北欧和波罗的海地区,采用加性修正法对Stokes公式进行最小二乘修正。新的精确的陆地、航空和船载重力测量、最近的全球重力场模型和稳态海洋环流探测器(GOCE)以及每个区域的详细数字地形模型被用于计算这个新的大地水准面模型。通过将该模型与每个国家的全球导航卫星系统(GNSS)数据进行比较,粗略地提出了对该模型误差的一些估计。在本文中,我们的目标是通过进行一些统计测试并找到适当的校正面来吸收每个国家的系统误差,从而更仔细地研究该模型的相对误差。我们的主要假设是GNSS/水准数据误差的现实性,我们将研究其对大地水准面模型误差估计的影响。结果表明,在瑞典、丹麦和芬兰,4参数校正面适合模拟重力和GNSS大地水准面高度差异的系统趋势,但在瑞典,应使用95%置信区间的过滤差异。挪威的7参数模型适用于过滤后的差异,置信区间为95%。基于所选择的校正面和我们新开发的区域迭代方差估计,瑞典、丹麦和挪威的NKG2015大地水准面模型误差置信区间分别为0 ~ 6.5 mm、1.8 ~ 5.2 mm和14.8 ~ 17.7 mm,置信水平为95%。我们无法估计芬兰的大地水准面误差,因为GNSS/水准高度的给定误差明显大于残差的大小。基于所选择的校正面和我们提出的局部方差估计,在瑞典、丹麦、挪威和芬兰,大地水准面平均误差分别为3.6、2.4、8.8和5.8 mm,置信区间为68%。
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来源期刊
Journal of Geodetic Science
Journal of Geodetic Science REMOTE SENSING-
CiteScore
1.90
自引率
7.70%
发文量
3
审稿时长
14 weeks
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