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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >A Time-Varying 3-D Displacement Model of the similar to 5.9-Year Westward Motion and its Applications for the Global Navigation Satellite System Positions and Velocities
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A Time-Varying 3-D Displacement Model of the similar to 5.9-Year Westward Motion and its Applications for the Global Navigation Satellite System Positions and Velocities

机译:类似于5.9年期间的3d位移模型及其对全球导航卫星系统位置和速度的应用

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摘要

To advance geodynamics and geophysical research, high precision Global Navigation Satellite System (GNSS) observations of velocity and position are needed. In this study, we construct a 3-D model of a similar to 5.9-year periodic signal for the Earth surface displacements. This model is mainly based on the determined time sequences and the Y-22 spatial pattern of this similar to 5.9-year periodic signal from the global Global Positioning System (GPS) observations. Based on the constructed model, we calculate synthetic temporal 3-D displacements on the Earth surface and the velocity changes, and we compare them to observed GPS displacements. Our results reveal that the similar to 5.9-year signal contributes to surface displacements and velocity fields. Maximum displacements for the N, E, and U components can reach up to 0.28, 0.55, and 1.69 mm, respectively; maximum velocity effects can up to 1.69 mm/year for the U component (depending on record length). For those studies which need millimeter or even submillimeter accuracy (e.g., tectonic deformations, glacial isostatic adjustment, and deformations caused by core motions), these effects cannot be simply ignored. Our results also confirm that the model we present here can heavily reduce the similar to 5.9-year signal in the original GPS time series. We suggest that our model should be used to pretreatment the GPS data at the observation level, which could improve signals used for geophysical or geodynamic interpretations.
机译:为了推进地球动力学和地球物理研究,需要高精度全球导航卫星系统(GNSS)的速度和位置观察。在这项研究中,我们构建了一个类似于5.9年的周期信号的3-D模型,用于地球表面位移。该模型主要基于所确定的时间序列和与来自全球全球定位系统(GPS)观测的5.9年的周期信号类似的时间序列和Y-22空间模式。基于构造模型,我们计算地面表面和速度变化的合成时间3-D位移,并将它们与观察到的GPS位移进行比较。我们的结果表明,类似于5.9年的信号有助于表面位移和速度场。 N,E和U组件的最大位移分别可以达到0.28,0.55和1.69 mm; U分量的最大速度效应可达1.69毫米/年(取决于记录长度)。对于那些需要毫米或甚至淹没精度的研究(例如,构造变形,冰川等静电调节和由核心运动引起的变形),不能简单地忽略这些效果。我们的结果还证实,我们在此提供的模型可以在原始GPS时间序列中严重降低类似于5.9年的信号。我们建议我们的模型应该用于预处理观察水平的GPS数据,这可以改善用于地球物理或地球动力解释的信号。

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