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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Remotely sensed variability of the suspended sediment concentration and its response to decreased river discharge in the Yangtze estuary and adjacent coast
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Remotely sensed variability of the suspended sediment concentration and its response to decreased river discharge in the Yangtze estuary and adjacent coast

机译:长江口及邻近沿海地区悬浮泥沙浓度的遥感变化及其对河流流量减少的响应

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Satellite observation is an excellent tool for exploring the variability of the suspended sediment concentration (SSC) of turbid estuarine and coastal waters. We used a recently developed semi-empirical radiative transfer model combined with a multi-wavelength switching algorithm for the SSC retrieval from MEdium Resolution Imaging Spectrometer (MERIS) satellite data. This method can successfully retrieve SSC from satellite data in turbid estuarine and coastal waters with a wide range of sediment concentrations (20-2500mgl~(-1)) and is robust for quantifying realistic patterns of the surface sediment dynamics. The seasonal and annual variability of the MERIS-derived SSC from 2003 to 2010 were analysed in this work. Five regions-of-interest (ROIs) in the Yangtze estuary and coast are included in the analysis: the upper estuary, the lower estuary, the outer estuary, the Hangzhou Bay and the Qidong shore. The results reveal that the SSC of the upper estuary has significant seasonal and annual variations in response to seasonal cycling and annual fluctuation of the river discharge. A long-term continuing decrease of river discharge may cause an overall decline of the SSC in the entire estuary and adjacent areas. The existence of horizontal exchanges of the sediments between the Yangtze estuary and the Jiangsu coast implies that the decreased fluvial sediment loads of the estuary may partially be compensated by supplementing contributions from other origins.
机译:卫星观测是探索混浊河口和沿海水域悬浮沉积物浓度(SSC)变异性的绝佳工具。我们使用了最近开发的半经验辐射传输模型,并结合了多波长切换算法,以从中分辨率成像光谱仪(MERIS)卫星数据中检索SSC。该方法可以成功地从浊度较高的河口和沿海水域的卫星数据中检索SSC,其沉积物浓度范围很广(20-2500mgl〜(-1)),并且对于量化表面沉积物动力学的现实模式具有鲁棒性。在这项工作中,分析了2003年至2010年MERIS衍生的SSC的季节和年度变化。分析中包括了长江口和沿海地区的五个感兴趣区域(ROI):上河口,下河口,外河口,杭州湾和启东海岸。结果表明,响应季节循环和河流流量的年度波动,上河口的南海夏季风有明显的季节和年度变化。河流流量的长期持续减少可能会导致整个河口和邻近地区的南南合作总体下降。长江口与江苏沿海之间沉积物水平交换的存在意味着,河口河道沉积物负荷的减少可以通过补充其他来源的贡献得到部分补偿。

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