地形剖面的时间序列建模

T. Sun, K. Alyass, Jinfeng Wei, D. Gorsich, M. Chaika, J. Ferris
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引用次数: 6

摘要

每次我们测量地形轮廓时,由于测量误差和测量车辆行驶的线性轨迹不可能每次都完全相同,我们都会得到一组不同的数据。然而,在不同时间从同一地形收集的数据应该具有相似的内在属性。因此,考虑地形剖面的统计建模是很自然的。在本文中,我们将使用时间序列模型,时间是到起点的距离。我们从比利时区块和Perryman3测试轨道接收数据。比利时块数据表现为均匀调制过程([7]),即它是确定性函数和平稳过程的乘积。剖面的建模可以通过估计确定性函数来完成,并使用已知的ARMA模型拟合平稳过程。Perryman3的数据更加不规则。我们必须使用内禀模态函数分解方法([2])。前几个固有模态函数可以用与比利时区块数据相同的方式建模。剩余部分是一个非常光滑的函数,我们可以把它看作是一个确定性函数。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Time Series Modeling of Terrain Profiles
Every time we measure the terrain profiles we would get a different set of data due to the measuring errors and due to the fact that the linear tracks on which the measuring vehicle travels can not be exactly the same every time. However the data collected at different times from the same terrain should share the similar intrinsic properties. Hence it is natural to consider statistical modeling of the terrain profiles. In this paper we shall use the time series models with time being the distance from the starting point. We receive data from the Belgian Block and the Perryman3 testing tracks. The Belgian Block data are shown to behave like a uniformly modulated process ([7]), i.e. it is the product of a deterministic function and a stationary process. The modeling of the profiles can be done by estimating the deterministic function and fit the stationary process with a well-known ARMA model. The Perryman3 data are more irregular. We have to use the intrinsic mode function decomposition method ([2]). The first few intrinsic mode functions could be modeled in the same way as the the Belgian Block data. The residue part is a very smooth function which we may consider as a deterministic function.
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