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Ocean surface monitoring based on GPS kinematic positioning

机译:基于GPS运动定位的海面监控

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In this paper, the conventional GPS kinematic positioning method and precise point positioning method for ocean surface monitoring are briefly presented and their corresponding pros and cons for sea level monitoring are also discussed. Then, algorithms for ocean surface parameter estimation from the GPS height component are introduced, which uses the spectral analysis method to extract sea level tide and sea wave parameters. A 48 hours GPS field data set by GPS buoy is used to evaluate the methods presented here. First, the height component analysis is performed to obtain the low-frequency and high-frequency signals which consist of ocean tide and wave components. Then, a wavelet transformation is performed to the high frequency series in order to detect the main wave period of about 10 second. The results show that GPS kinematic positioning technique can not only be used for ocean positioning but can also be used to monitor the ocean surface.
机译:本文还讨论了传统的GPS运动定位方法和海洋表面监测的精确点定位方法及其对应的海平监测的相应优点和缺点。然后,介绍了来自GPS高度分量的海洋表面参数估计的算法,其使用光谱分析方法提取海平潮和海波参数。 GPS浮标设置的48小时GPS字段数据用于评估此处提供的方法。首先,执行高度分量分析以获得由海潮和波部件组成的低频和高频信号。然后,对高频系列执行小波变换,以检测大约10秒的主波周期。结果表明,GPS运动学定位技术不仅可以用于海洋定位,而且还可用于监测海洋表面。

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