测绘学报 ›› 2023, Vol. 52 ›› Issue (11): 1835-1843.doi: 10.11947/j.AGCS.2023.20220203

• 大地测量学与导航 • 上一篇    下一篇

邻近海底基准站坐标时序联合处理模型

孙悦1,2, 薛树强2, 韩保民1, 肖圳1,2   

  1. 1. 山东理工大学建筑工程与空间信息学院, 山东 淄博 255049;
    2. 中国测绘科学研究院, 北京 100036
  • 收稿日期:2022-04-02 修回日期:2023-06-07 发布日期:2023-12-15
  • 通讯作者: 薛树强 E-mail:xuesq@casm.ac.cn
  • 作者简介:孙悦(1997-),女,硕士,研究方向为水下导航定位应用。E-mail:iamssunyuea@163.com
  • 基金资助:
    崂山实验室科技创新项目(LSKJ202205100;LSKJ202205105);国家重点研究计划(No.2020YFB0505802)

Multi-station joint processing model for seafloor geodetic coordinate time series

SUN Yue1,2, XUE Shuqiang2, HAN Baomin1, XIAO Zhen1,2   

  1. 1. School of Civil Engineering and Geomatics, Shandong University of Technology, Zibo 255049, China;
    2. Chinese Academy of Surveying and mapping, Beijing 100036, China
  • Received:2022-04-02 Revised:2023-06-07 Published:2023-12-15
  • Supported by:
    Science and Technology Innovation Project Funded by Laoshan Laboratory (Nos. LSKJ202205100;LSKJ202205105);The National Key Research and Development Program of China (No. 2020YFB0505802)

摘要: 海底基准站复测观测可用于海底构造和海底地震等灾害研究。然而,受观测条件和供电等因素影响,难以实现长时间不间断观测。为解决时间序列观测中新旧海底基准站替换位移补偿和站点偏移量计算问题,可采用中心点法求取相对于海底基准站网的虚拟中心点坐标的位移量,进而构造海底基准坐标时序,以监测海底构造运动。针对相同的问题,本文借鉴地球参考框架维持方式,直接利用可能存在间断的海底基准站网时序观测数据,提出了基于参考协议历元的海底基准坐标时序多站联合处理模型,即在一个区域基准站网内,各站点坐标作为局部参数,而站速度作为公共参数。本文方法适合于海底参考框架的建立与动态维持,利于对区域网内各站点坐标时序实施精细质量控制。结果表明,本文方法可以代替中心点法,且抗差估计结果更为可靠,与中心点法确定的海底基准站年速度估计之间的差值平均为3 mm/a,可为国家海底空间基准维持提供一种途径。

关键词: 海底大地测量, 地壳运动, 站速度, 抗差估计, 灾害监测

Abstract: The repeated observation of seafloor geodetic network can be used to study the seafloor plate technic and the process of marine disaster such as seafloor earthquake. However, affected by observation condition, power supply and other factors, it is hard to achieve continuous observation for a long time. To solve the displacement compensation and site offset calculation problems in the replacement of old and new underwater geodetic stations in time series observations, the center point method can be used to calculate the displacement relative to the virtual center point coordinates of the underwater geodetic station network, and then construct the underwater geodetic coordinate the series to monitor underwater tectonic movement. For the same problem. Referring to the maintenance way of the terrestrial reference frame, we directly use the time series observation data of the seafloor geodetic network that may have discontinuities, and propose a multi station joint processing model of the seafloor geodetic coordinates based on the reference protocol epoch, in other words, in a regional geodetic network the coordinates of each station are treated as local parameters, and the velocity is used as a common parameter. The new proposed method is not only suitable for the geodetic dynamic reference frame maintenance, but also can be conducive to the implementation of fine quality control of the coordinate time series of each geodetic station in the regional network. The experimental results show that, the difference of annual velocity estimation difference of seafloor geodetic network between the two methods is about 3 mm/a. The new proposed method is a substitute for the center point method, and the robust estimation results are more reliable. This study provides a way for maintaining the national seafloor space benchmark.

Key words: seafloor geodesy, plate movement, station velocity, robust estimation, disaster monitoring

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