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首页> 外文期刊>Annals Of Geophysics >Geophysical interpretation of GPS loading deformation over western Europe using GRACE measurements
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Geophysical interpretation of GPS loading deformation over western Europe using GRACE measurements

机译:利用GRACE测量对西欧GPS载荷变形的地球物理解释

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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:我们对欧洲36个国际GNSS服务(IGS)站的重力恢复和气候实验(GRACE)观测到的表面质量载荷所预测的全球定位系统(GPS)高度残差和垂直位移进行了10多年的分析。在GPS和GRACE测量中,季节性表面位移(主要是由于大气和水文负荷)是很重要的。在较长的时间范围内,我们基于空间研究中心(CSR)的05 GRACE版本数据进行的新分析显示,GPS和GRACE之间的一致性比以前的研究有了很大改善,不仅针对年度信号,而且针对年度信号。在删除GRACE派生的垂直位移后,大多数站点的GPS高度残差序列显示出减小的加权均方根(WRMS),这归因于GPS和GRACE数据产品的精度提高。此外,我们证明了使用GRACE卫星重力观测研究GRACE估算中减少泄漏偏差的必要性,以研究表面载荷变形。

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