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首页> 外文期刊>Journal of Geodesy >Estimates of ocean tide loading displacements and its impact on position time series in Hong Kong using a dense continuous GPS network
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Estimates of ocean tide loading displacements and its impact on position time series in Hong Kong using a dense continuous GPS network

机译:利用密集连续GPS网络估算香港的潮汐载荷位移及其对位置时间序列的影响

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摘要

Three-dimensional ocean tide loading (OTL) displacements of eight diurnal and semidiurnal constituents at 12 sites in Hong Kong were estimated using 3-7 years of continuous global positioning system (GPS) observations. OTL displacements were estimated using the precise point positioning (PPP) technique on a daily basis and then combined. The OTL displacements obtained by GPS were compared with predictions using seven recent global ocean tide models. The effect of OTL displacements on GPS position time series was also investigated. The study shows that the GPS-derived OTL displacements (excluding K1 and K2 constituents) agree best with those predicted by the GOT4.7 and NAO99b models. The GPS/model agreement is generally at the sub-millimeter level, except for S2, K1, and K2 constituents with relatively large errors. After systematic biases between the GPS and model values are removed, the misfits of all sites for M2, S2, N2, 01, P1, and Q1 are less than 0.5 and 1.0 mm in the horizontal and vertical components, respectively, while larger misfits (within 2.5 mm) are observed for Kl and K2. Integer ambiguity fixing slightly improves the east component of OTL displacement estimates. The study also finds that GPS-derived OTL corrections, instead of model predicts, can be used in daily data processing with the exception of K1 and K2. Including K2 corrections, a secular vertical rate of up to 1 mm/year in position time series can be induced, which needs to be confirmed by further studies.
机译:使用3-7年的连续全球定位系统(GPS)观测值,估算了香港12个地点的8个昼夜和半昼间成分的三维海潮载荷(OTL)位移。每天使用精确点定位(PPP)技术估算OTL位移,然后进行组合。通过GPS获得的OTL位移与使用七个最新全球海潮模型的预测结果进行了比较。还研究了OTL位移对GPS位置时间序列的影响。研究表明,GPS衍生的OTL位移(不包括K1和K2成分)与GOT4.7和NAO99b模型预测的位移最吻合。 GPS /模型协议通常处于亚毫米级别,但误差较大的S2,K1和K2组成部分除外。消除GPS与模型值之间的系统性偏差后,水平和垂直分量中M2,S2,N2、01,P1和Q1的所有位置的失配分别小于0.5和1.0 mm,而较大失配(对于K1和K2观察到2.5mm以内)。整数歧义修复会稍微改善OTL位移估计的东部部分。这项研究还发现,除了K1和K2之外,GPS衍生的OTL校正(而不是模型预测)可用于日常数据处理。包括K2校正在内,在位置时间序列上可以诱发高达1毫米/年的长期垂直速率,这需要进一步的研究加以证实。

著录项

  • 来源
    《Journal of Geodesy》 |2009年第11期|999-1015|共17页
  • 作者单位

    Department of Land Surveying and Geo-Informatics, The Hong Kong Polytechnic University, Hung Horn, Kowloon, Hong Kong, China;

    Department of Land Surveying and Geo-Informatics, The Hong Kong Polytechnic University, Hung Horn, Kowloon, Hong Kong, China;

    Department of Land Surveying and Geo-Informatics, The Hong Kong Polytechnic University, Hung Horn, Kowloon, Hong Kong, China;

    Department of Land Surveying and Geo-Informatics, The Hong Kong Polytechnic University, Hung Horn, Kowloon, Hong Kong, China;

    Department of Surveying Engineering, Southwest Jiaotong University, 610031 Chengdu, Sichuan. China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    GPS; ocean tide loading (OTL); ocean tide model; error propagation; Hong Kong;

    机译:全球定位系统;海洋潮汐负荷(OTL);海潮模型;错误传播;香港;

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