首页> 外文会议>Proceedings of the 17th international technical meeting of the Satellite Division of the Institute of Navigation (ION GNSS 2004) >Tidal Height Retrieval Using Globally Corrected GPS in the Amundsen Gulf Region of the Canadian Arctic
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Tidal Height Retrieval Using Globally Corrected GPS in the Amundsen Gulf Region of the Canadian Arctic

机译:使用全球校正的GPS反演加拿大北极地区阿蒙森海湾地区的潮高

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摘要

The recent evolution of global Wide Area Differential GPS (WADGPS) networks has greatly increased the already high level of interest in GPS technologies by the hydrographic community. The aim of this paper is to evaluate one of these WADGPS systems, the C & C Technologies Globally Corrected GPS (GcGPS) C-Nav, as an instrument for tidal height retrieval in the Canadian Arctic. The C-Nav receiver was mounted aboard the Canadian Coast Guard Ship (CCGS) Amundsen for her 14-month over-wintering expedition in the Northwest Passage. C-Nav height data were collected in Franklin Bay, North West Territories, over February to April 2004. Data were collected over a 40-day period to ensure the capture of all significant wavelength tidal effects. rnAs a ‘true’ vertical reference, Knudsen K320 sub-bottom profiling sonar depth data were collected. The 1 Hz CNav data were processed and decimated down to 6-minute epochs, thus speeding the filter processing to obtain realtime data latency. Over the course of the research period, the standard deviation of the C-Nav data was 4.3 cm, when compared to the ‘true’ tidal signature given by the K320. This level of positioning is commensurate with International Hydrographic Organization (IHO) Special Order surveys. In addition, the benefits of the C-Nav solution were apparent in capturing the phase lag of the tides due to sea ice effects. Tidal predictions using common software applications such as the Unix based program Xtide, yielded standard deviations of 5.3 cm.
机译:全球广域差分GPS(WADGPS)网络的最新发展极大地增加了水文界对GPS技术的高度关注。本文的目的是评估其中一种WADGPS系统,即C&C技术全球校正GPS(GcGPS)C-Nav,作为加拿大北极潮汐高度检索的一种手段。 C-Nav接收器安装在加拿大海岸警卫队(CCGS)阿蒙森号上,进行了为期14个月的西北通道冬季越冬之旅。 2004年2月至2004年4月在西北地区富兰克林湾收集了C-Nav高度数据。在40天的时间内收集了数据,以确保捕获所有重要的潮汐效应。 rn作为“真实”垂直参考,我们收集了Knudsen K320底部轮廓声纳深度数据。对1 Hz CNav数据进行处理并抽取到6分钟的时间,从而加快了滤波器处理以获得实时数据延迟的速度。在研究期间,与K320给出的“真实”潮汐特征相比,C-Nav数据的标准偏差为4.3 cm。此定位级别与国际水文组织(IHO)的特别命令调查相称。此外,C-Nav解决方案的优势在捕获由于海冰效应引起的潮汐相位滞后方面显而易见。使用常见的软件应用程序(例如,基于Unix的程序Xtide)进行潮汐预测的标准差为5.3 cm。

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