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Chapter 2 Ocean Tidal Loading Effects to Displacements at GNSS Sites

机译:第2章海洋潮汐负荷对GNSS站点位移的影响

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Ocean tidal loading (OTL) effects to displacements should be considered during GNSS precise positioning. Especially, along with the shift of geodesy from mainland to ocean, the OTL corrections to displacements play more and more important roles in precise positioning. The approaches to resolve OTL effects in precise GNSS data processing software GAMIT are that, either directly reading out the amplitudes and phases of several main tidal constituents (also called tidal coefficients) at site from file station.oct, or interpolating the site's tidal coefficients from global grid file grid.oct. It's not ideal to modify the OTL effects in China mainland (especially in coast areas, islands and reefs) using GAMIT directly, because of tidal coefficients' errors or the limitations of tracking stations' distribution. This paper detailed describes the OTL effects theories to displacements based on convolution integration approach about OTL and Green's functions. Numerical integration of OTL is performed using the Gauss quadrature method and the integration areas are separated to inner zone and outer zone. A newest 2' × 2' resolutions local ocean tidal model of the East China Sea and South China Sea was adopted for inner zone, and a global model TPXO7.2 for the outer zone. Some OTL corrections to displacements at coast GNSS sites were computed, and which were applied to the GNSS data processing. The estimation of amplitudes and phases for the main tidal constituent M2 were acquired at some sites, variation functions changed with time for displacement were constructed. Numerical tests show that, the displacements at coast sites are bigger than those at inland sites, amplitudes of local loading on displacements reach the order of centimetre. If the amplitudes and phases of tidal constituents calculated by this method are appended into the station.oct file, the baselines' accuracies will be improved greatly for GAMIT software. Not only the OTL corrections but also suitable ocean tidal models and tide constituents should be taken into account in GNSS data analyses.
机译:在GNSS精确定位期间,应考虑海洋潮汐载荷(OTL)对位移的影响。特别是,随着大地测量学从大陆转移到海洋,将OTL校正到位移在精确定位中起着越来越重要的作用。在精确的GNSS数据处理软件GAMIT中解决OTL效应的方法是,要么直接从File Station.oct读取站点上几个主要潮汐成分(也称为潮汐系数)的幅度和相位,要么从File Station.oct中插入站点的潮汐系数。全局网格文件grid.oct。由于潮汐系数的误差或跟踪站分布的局限性,直接使用GAMIT修改中国大陆(尤其是沿海地区,岛屿和礁石)的OTL效果并不理想。本文详细介绍了基于OTL和格林函数的卷积积分方法的OTL对位移的影响理论。使用高斯求积法对OTL进行数值积分,积分区域分为内部区域和外部区域。内部区域采用了最新的2'×2'分辨率东海和南海局部海洋潮汐模型,外部区域采用了全球模型TPXO7.2。计算了对海岸GNSS站点位移的一些OTL校正,并将其应用于GNSS数据处理。在某些地点获取了主要潮汐分量M2的振幅和相位估计,并构建了随时间变化的位移函数。数值试验表明,海岸点的位移大于内陆点的位移,局部载荷的振幅达到厘米级。如果将通过此方法计算出的潮汐成分的幅度和相位附加到station.oct文件中,则GAMIT软件将大大提高基线的准确性。在GNSS数据分析中,不仅应考虑OTL校正,还应考虑合适的海洋潮汐模型和潮汐成分。

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