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Estimation of tidally influenced estuarine river discharge from space using along-track InSAR technology: A model-based feasibility study

机译:利用沿轨InsaR技术估算潮汐影响的河口河流流量:基于模型的可行性研究

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摘要

We discuss the potential of the along-track interferometric synthetic aperture radar (along-track InSAR, ATI) technique for monitoring tidally influenced estuarine river discharge from space. To observe river discharge using ATI, surface velocity measurements need to be converted to depth-integrated velocity to apply empirical discharge models and, possibly aliased, tidal signals need to be removed. Problems may also arise from the fact that ATI velocity observations generally are not in the along-flow direction, and from uncertainties in applied empirical discharge models. To quantify the degree to which river discharge can be inferred from ATI data, output from a high-resolution numerical model of the Elbe estuary serves here as the basis for simulated observations of a TerraSAR-X-like satellite mission as well as simulated ground truth against which retrieved transports are tested. Results show that with only the additional information of the river widths, instantaneous discharge estimates can be obtained from ATI-derived velocities. To retrieve mean discharges from a number of instantaneous measurements at different tidal phases, we fit time series of the tidal components M-2 and K-1 to the data by amplitude and phase adjustment and subtract them. We demonstrate the successful application of such a mean-value estimator for calculating net discharges. A simulated TerraSAR-X sampling scenario provides discharge estimates for the Elbe estuary with accuracies in the range of 20-30%, comparable in quality to commonly used ground-based noncontact discharge measurements. The proposed satellite-based monitoring approach, therefore, provides a promising new method for river discharge estimates in estuaries, especially in regions where onsite measurements are not possible or data are not accessible.
机译:我们讨论了沿径迹干涉式合成孔径雷达(沿径迹InSAR,ATI)技术的潜力,该技术可监测潮汐影响的河口从太空的排放。为了使用ATI观测河流流量,需要将表面速度测量值转换为深度积分速度以应用经验流量模型,并且可能需要消除潮汐信号。 ATI速度观测值通常不在沿流方向的事实,以及应用的经验排放模型的不确定性,也可能引起问题。为了量化可从ATI数据推断出河流流量的程度,此处易北河河口高分辨率数值模型的输出将作为类似TerraSAR-X卫星任务的模拟观测以及模拟地面真相的基础将针对其测试检索到的传输。结果表明,仅使用河流宽度的附加信息,就可以从ATI得出的速度获得瞬时流量估算值。为了从不同潮汐相位的大量瞬时测量值中检索出平均流量,我们通过幅度和相位调整将潮汐分量M-2和K-1的时间序列拟合到数据中,并减去它们。我们证明了这种均值估算器在计算净排放量方面的成功应用。模拟的TerraSAR-X采样方案可为易北河河口提供流量估算,其准确度在20%至30%之间,其质量可与常用的基于地面的非接触式流量测量相媲美。因此,拟议的基于卫星的监测方法为河口,尤其是在无法进行现场测量或无法获得数据的地区中的河流流量估算提供了一种有希望的新方法。

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