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Improved vertical displacements induced by a refined thermal expansion model and its quantitative analysis in GPS height time series

机译:改进了通过GPS高度时间序列的精制热膨胀模型引起的垂直位移及其定量分析

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There are apparent seasonal variations in GPS height time series, and thermal expansion is considered to be one of the potential geophysical contributors. The displacements introduced by thermal expansion are usually derived without considering the annex height and underground part of the monument (e.g. located on roof or top of the buildings), which may bias the geophysical explanation of the seasonal oscillation. In this paper, the improved vertical displacements are derived by a refined thermal expansion model where the annex height and underground depth of the monument are taken into account, and then 560 IGS stations are adopted to validate the modeled thermal expansion (MTE) displacements. In order to evaluate the impact of thermal expansion on GPS heights, the MTE displacements of 80 IGS stations with less data discontinuities are selected to compare with their observed GPS vertical (OGV) displacements with the modeled surface loading (MSL) displacements removed in advance. Quantitative analysis results show the maximum annual and semiannual amplitudes of the MTE are 6.65 mm (NOVJ) and 0.51 mm (IISC), respectively, and the maximum peak-to-peak oscillation of the MTE displacements can be 19.4 mm. The average annual amplitude reductions are 0.75 mm and 1.05 mm respectively after removing the MTE and MSL displacements from the OGV, indicating the seasonal oscillation induced by thermal expansion is equivalent to 75% of the impact of surface loadings. However, there are rarely significant reductions for the semiannual amplitude. Given the result in this study that thermal expansion can explain 17.3% of the annual amplitude in GPS heights on average, it must be precisely modeled both in GPS precise data processing and GPS time series analysis, especially for those stations located in the middle and high latitudes with larger annual temperature oscillation, or stations with higher monument.
机译:GPS高度时间序列存在明显的季节变化,并且热膨胀被认为是潜在的地球物理贡献者之一。通过热膨胀引入的位移通常导出,而不考虑纪念碑的附件高度和地下部分(例如位于建筑物的屋顶或顶部),这可能会偏离季节性振荡的地球物理解释。在本文中,改进的垂直位移由精制的热膨胀模型导出,其中纪念碑的附件高度和地下深度被考虑,然后采用560个IGS站来验证建模的热膨胀(MTE)位移。为了评估热膨胀对GPS高度的影响,选择具有较少数据不连续的80个IGS站的MTE位移以与预先除去的模型表面负载(MSL)位移的观察到的GPS垂直(OGV)位移进行比较。定量分析结果显示MTE的最高年度和半壮大分别为6.65毫米(新闻)和0.51毫米(IISC),MTE位移的最大峰峰振荡可以是19.4毫米。从OGV移除MTE和MSL位移后,平均年度幅度减小分别为0.75毫米,1.05毫米,表示热膨胀诱导的季节性振荡相当于表面负荷的影响的75%。然而,半年幅度很少减少。鉴于该研究的结果,热膨胀可以平均解释GPS高度的年度幅度的17.3%,必须在GPS精确数据处理和GPS时间序列分析中精确建模,特别是对于位于中高的那些电台年度温度振荡的纬度或纪念碑高等纪念碑。

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