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Joint analysis of seasonal oscillations derived from GPS observations and hydrological loading for mainland China

机译:GPS观测资料与中国大陆水文负荷的季节性波动联合分析

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摘要

Hydrological loading effects are one of the principal sources of the seasonal oscillations in GPS position time series, and they should be taken into account for improving GPS system accuracy. In this study, the daily vertical position time series of 23 GPS stations derived from the Crustal Movement Observation Network of China (CMONOC) are used to investigate the hydrological loading contributors of seasonal oscillations in GPS observations. The hydrological loading deformations at each GPS station are estimated by the Global Land Surface Discharge Model (LSDM). The result of period analysis suggests that the hydrological loading primarily results in the annual oscillation in GPS observations. Therefore, Multichannel Singular Spectrum Analysis (MSSA) is utilized to derive the annual signal from GPS observations and LSDM-derived deformations simultaneously for each GPS station. Compared with Singular Spectrum Analysis (SSA), the percentage of the variance of the annual signal estimated by MSSA and SSA differs by 6% on average, indicating that MSSA can effectively separate annual signal from other signals and clear noise. Meanwhile, Cross Wavelet Transform (XWT) is performed to measure the correlation and phase relationship between GPS observations and LSDM-derived deformations in the time-frequency space. The result demonstrates that the hydrological loading can only explain the annual oscillation in GPS observations at 5 stations (namely LHAS, LUZH, KMIN, QION, and XIAG) well. For the most GPS stations, other factors (e.g., other geophysical factors, hydrological modeling errors, and systematic errors) and hydrological loading jointly contribute to the annual oscillation in GPS observations. After hydrological loading correction, the Root Mean Square (RMS) values of GPS observations are reduced at 15 stations, especially for the GPS stations located in regions with significant water storage variations (up to 2.46 mm at KMIN). Moreover, the percentage of the variance of the annual signal estimated by MSSA correlates well with the RMS reduction, implying that the RMS reduction may be related to the annual signal derived from hydrological loading deformations. (C) 2018 COSPAR. Published by Elsevier Ltd. All rights reserved.
机译:水文负荷效应是GPS位置时间序列中季节性振荡的主要来源之一,为提高GPS系统的精度应将其考虑在内。在这项研究中,使用来自中国地壳运动观测网络(CMONOC)的23个GPS站的每日垂直位置时间序列,来研究GPS观测中季节性振荡的水文负荷贡献者。每个GPS站的水文荷载变形通过全球陆面排水模型(LSDM)估算。周期分析的结果表明,水文负荷主要导致GPS观测中的年度振荡。因此,多通道奇异频谱分析(MSSA)用于为每个GPS站同时从GPS观测值和LSDM衍生的变形中导出年度信号。与奇异频谱分析(SSA)相比,MSSA和SSA估计的年度信号方差百分比平均相差6%,这表明MSSA可以有效地将年度信号与其他信号分开并清除噪声。同时,执行交叉小波变换(XWT)来测量时空空间中GPS观测值与LSDM衍生形变之间的相关性和相位关系。结果表明,水文负荷仅能解释5个站(即LHAS,LUZH,KMIN,QION和XIAG)的GPS观测的年振荡。对于大多数GPS站而言,其他因素(例如其他地球物理因素,水文模型误差和系统误差)和水文负荷共同导致GPS观测值的年度振荡。经过水文荷载校正后,GPS观测值的均方根(RMS)值在15个站处减小,尤其是对于位于具有显着蓄水量变化的区域(KMIN处最大为2.46 mm)的GPS站。此外,由MSSA估算的年度信号的方差百分比与RMS降低有很好的相关性,这意味着RMS的降低可能与从水文荷载变形得出的年度信号有关。 (C)2018年COSPAR。由Elsevier Ltd.出版。保留所有权利。

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