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Vertical deformations from homogeneously processed GRACE and global GPS long-term series

机译:均匀处理的GRACE和全球GPS长期序列的垂直变形

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摘要

Temporal variations in the geographic distribution of surface mass cause surface displacements. Surface displacements derived from GRACE gravity field coefficient time series also should be observed in GPS coordinate time series, if both time series are sufficiently free of systematic errors. A successful validation can be an important contribution to climate change research, as the biggest contributors to mass variability in the system Earth include the movement of oceanic, atmospheric, and continental water and ice. In our analysis, we find that if the signals are larger than their precision, both geodetic sensor systems see common signals for almost all the 115 stations surveyed. Almost 80% of the stations have their signal WRMS decreased, when we subtract monthly GRACE surface displacements from those observed by GPS data. Almost all other stations are on ocean islands or small peninsulas, where the physically expected loading signals are very small. For a fair comparison, the data (79 months from September 2002 to April 2009) had to be treated appropriately: the GPS data were completely reprocessed with state-of-the-art models. We used an objective cluster analysis to identify and eliminate stations, where local effects or technical artifacts dominated the signals. In addition, it was necessary for both sets of results to be expressed in equivalent reference frames, meaning that net translations between the GPS and GRACE data sets had to be treated adequately. These data sets are then compared and statistically analyzed: we determine the stability (precision) of GRACE-derived, monthly vertical deformation data to be ~ 1.2 mm, using the data from three GRACE processing centers. We statistically analyze the mean annual signals, computed from the GPS and GRACE series. There is a detailed discussion of the results for five overall representative stations, in order to help the reader to link the displayed criteria of similarity to real data. A series of tests were performed with the goal of explaining the remaining GPS-GRACE residuals.
机译:表面质量地理分布的时间变化会导致表面位移。如果两个时间序列都没有系统误差,则应在GPS坐标时间序列中观察到从GRACE重力场系数时间序列得出的表面位移。成功的验证可能是对气候变化研究的重要贡献,因为对地球系统质量变化最大的贡献是海洋,大气和大陆水和冰的运动。在我们的分析中,我们发现,如果信号大于其精度,则两个大地传感器系统都将在几乎所有被调查的115个站点中看到通用信号。当我们从GPS数据观测到的月度GRACE地面位移中减去时,几乎80%的测站的信号WRMS减小。几乎所有其他站点都位于大洋岛屿或小半岛上,那里的物理预期加载信号非常小。为了进行公平的比较,必须对数据(从2002年9月到2009年4月的79个月)进行适当处理:使用最新模型对GPS数据进行了完全重新处理。我们使用客观的聚类分析来识别和消除站点,在站点中局部效果或技术伪影主导了信号。此外,有必要在等效的参考框架中表示两组结果,这意味着必须适当处理GPS和GRACE数据集之间的净翻译。然后对这些数据集进行比较并进行统计分析:我们使用来自三个GRACE处理中心的数据,确定GRACE衍生的每月垂直变形数据的稳定性(精度)为〜1.2 mm。我们对GPS和GRACE系列计算出的年均信号进行统计分析。对五个总体代表站的结果进行了详细讨论,以帮助读者将显示的相似性标准链接到实际数据。为了说明其余的GPS-GRACE残差,进行了一系列测试。

著录项

  • 来源
    《Journal of Geodesy》 |2011年第5期|p.291-310|共20页
  • 作者单位

    OHB-System AG, Universitatsallee 27-29, 28359 Bremen, Germany;

    Institut fur Astronomische und Physikalische Geodasie, Technische Universitat Miinchen, Arcisstr. 21, 80333 Munich, Germany;

    Faculty of Science, Technology, and Communication, University of Luxembourg, 6, rue Richard Coudenhove-Kalergi, 1359 Luxembourg, Luxembourg;

    Institute of Geodesy and Geoinformation, University of Bonn, Nussallee 17, 53115 Bonn, Germany;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    satellite geodesy; earth system; GRACE; GPS; mass transport; surface deformation;

    机译:卫星大地测量地球系统恩典;全球定位系统;大众运输;表面变形;

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