首页> 外文会议>China satellite navigation conference >Tide Height Inversion and Accuracy Analysis Based on GNSS-MR Technology
【24h】

Tide Height Inversion and Accuracy Analysis Based on GNSS-MR Technology

机译:基于GNSS-MR技术的潮高反演与精度分析

获取原文

摘要

The tide height of offshore waters is an indispensable marine geographic information data for marine traffic, offshore environmental management, and marine disaster warning and forecasting. Recently years, with the advantages of low power consumption and low cost, the Global Navigation Satellite System Multipath Reflection (GNSS-MR) technology has become an emerging technical method of tide height measurement. In this article, the observation files of SC02 station in 2018 in Washington state of United States is used to retrieve the distance in vertical direction from antenna phase center to sea surface by using the change of signal-to-noise ratio (SNR) caused by the multipath effect of navigation satellite signal. Afterwards, the elevation based on International Terrestrial Reference Frame (ITRF) is converted to the elevation based on the Mean Lower Low Water (MLLW). And then the tide height of each inversion time relative to MLLW is obtained. Finally, the retrieved tide height is compared and analyzed with the tide height offered by the tide gauge station named FRIDAY HARBOR. The results show that the mean error of the two is about -12 cm, the root mean square error is about 15 cm, and the correlation coefficient is about 0.98. Overall, the retrieved tide height agrees well with the measured tide height. Hence, the tide height retrieved by GNSS-MR technology can make up for the lack of ocean observation data in the coastal waters and plays an important role in marine scientific research.
机译:海上水域的潮高是海洋交通,近海环境管理以及海洋灾害预警和预测必不可少的海洋地理信息数据。近年来,以低功耗和低成本为优势,全球导航卫星系统多径反射(GNSS-MR)技术已成为潮汐高度测量的新兴技术方法。本文利用美国华盛顿州SC02站2018年的观测文件,通过计算由以下原因引起的信噪比(SNR)的变化来检索天线相位中心到海面在垂直方向上的距离导航卫星信号的多径效应。然后,将基于国际陆地参考系(ITRF)的海拔转换为基于平均低水位(MLLW)的海拔。然后获得每个反演时间相对于MLLW的潮高。最后,将检索到的潮汐高度与名为FRIDAY HARBOR的潮汐仪站提供的潮汐高度进行比较和分析。结果表明,两者的平均误差约为-12 cm,均方根误差约为15 cm,相关系数约为0.98。总体而言,检索到的潮汐高度与测得的潮汐高度高度吻合。因此,利用GNSS-MR技术获取的潮高可以弥补沿海水域海洋观测数据的不足,并在海洋科学研究中发挥重要作用。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号