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Geophysical interpretation of GPS loading deformation over western Europe using GRACE measurements

机译:基于GRACE测量的西欧GPS加载变形的地球物理解读

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摘要

We analyze more than 10 years of Global Positioning System (GPS) height residuals and vertical displacements predicted from surface mass loading observed by the Gravity Recovery and Climate Experiment (GRACE) for 36 International GNSS Service (IGS) stations over Europe. Seasonal surface displacements, mostly due to atmospheric and hydrological loading, are significant in both GPS and GRACE measurements. With an extended time period, our new analysis based on release 05 GRACE data from Center for Space Research (CSR) shows considerably improved agreement between GPS and GRACE than that from previous studies, for not only annual but also interannual signals. The GPS height residual series at most stations exhibit reduced weighted root-mean-squares (WRMS) after removing GRACE-derived vertical displacements, which is attributed to improved accuracy of both GPS and GRACE data products. Furthermore, we demonstrate the necessity of reducing leakage bias in GRACE estimates for the study of surface loading deformation using GRACE satellite gravity observations.
机译:我们分析了超过10年的全球定位系统(GPS)高度残留物和垂直位移,从欧洲的36个国际GNSS服务(IGS)站所观察到的重力恢复和气候实验(Grace)观察到的表面大量负载。季节性表面位移,主要是由于大气和水文加载,在GPS和Grace测量中都是显着的。通过延长的时间段,我们的新分析来自空间研究中心(CSR)的05宽度数据(CSR)显示了GPS和Grace之间的同意,而不是从以前的研究,不仅是年度的年度,而且还有年度依赖于年度信号。在除去宽限导出的垂直位移之后,大多数站的GPS高度残差系列在旨在提高GPS和Grace数据产品的准确性后,大多数站点都表现出减少的加权根平均正方形(WRM)。此外,我们展示了使用Grace卫星重力观测对表面装载变形研究减少泄漏偏差的必要性。

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