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Lake Level Estimation Based on CryoSat-2 SAR Altimetry and Multi-Looked Waveform Classification

机译:基于CryoSat-2 SAR测高和多波形分类的湖泊水位估计

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In this study, reliable water levels for four lakes are estimated based on an innovative processing strategy using a semi-automatic CryoSat-2 Synthetic Aperture Radar (SAR) multi-looked waveform classification. The selection of valid water returns is an essential step in inland altimetry applications. In order to identify reliable observations allowing for an accurate retracking, an unsupervised classification method for CryoSat-2 SAR multi-looked waveforms has been developed based on the k-mean algorithm. With this approach, changes in the water surface extent or surrounding inundation areas can be taken into account. In addition, a modified version of the Improved Threshold Retracker is developed in order to obtain optimal results for the lake heights. The used method is based on the identification of the optimal sub-waveform by employing height thresholds. The validation of the derived CryoSat-2 SAR time series with in-situ gauging data yields root mean square (RMS) differences between 3 and 90 cm for the different lakes. Compared to modeled CryoSat-2 water heights derived according to the approach used in the AltWater database our water level time series are slightly improved in terms of RMS accuracy but they contain more gaps due to the lack of reliable observations. In comparison with classical radar altimeter missions such as Envisat or Jason-2, the SAR-based time series show smaller RMS differences for the small lakes but larger RMS differences for the large lakes covered by multiple repeat missions. The presented innovative processing strategy can be easily adopted to other satellite altimetry SAR data such as from the new Sentinel-3 mission.
机译:在这项研究中,基于创新的处理策略,使用半自动CryoSat-2合成孔径雷达(SAR)多元波形分类,估算了四个湖泊的可靠水位。在内陆测高应用中,有效回水的选择是必不可少的步骤。为了识别可靠的观测值以实现准确的重新跟踪,基于k均值算法,开发了一种针对CryoSat-2 SAR多重观测波形的无监督分类方法。通过这种方法,可以考虑水面范围或周围淹没区域的变化。此外,还开发了改进阈值跟踪器的改进版本,以便获得湖泊高度的最佳结果。所使用的方法基于通过采用高度阈值识别最佳子波形的方法。用原位测量数据对导出的CryoSat-2 SAR时间序列进行验证,得出不同湖泊的3到90 cm的均方根(RMS)差。与根据AltWater数据库中使用的方法得出的模拟CryoSat-2水高相比,在RMS精度方面,我们的水位时间序列略有改善,但由于缺乏可靠的观察,它们之间的差距更大。与Envisat或Jason-2等经典雷达高度计任务相比,基于SAR的时间序列显示小湖泊的RMS差异较小,而多次重复任务覆盖的大型湖泊的RMS差异较大。提出的创新处理策略可以轻松地应用于其他卫星测高SAR数据,例如来自新的Sentinel-3任务的数据。

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