首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Retrieval of suspended sediment concentrations in large turbid rivers using Landsat ETM plus : an example from the Yangtze River, China
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Retrieval of suspended sediment concentrations in large turbid rivers using Landsat ETM plus : an example from the Yangtze River, China

机译:使用Landsat ETM plus反演大型浑浊河流中的悬浮沉积物浓度:以中国长江为例

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摘要

Suspended sediment concentration (SSC) is a critical parameter in the study of river sediment transport and water quality variation, but traditional measurement methods are costly and time-consuming. This paper is focused on presenting a methodology that may be useful in estimating SSC which is of key importance in process geomorphology and hydrology. In previous studies, remote sensing has been applied to estimate the SSC of sea waters as well as low turbid inland waters like lakes, reservoirs and short river reaches visible within a single Landsat satellite image coverage. Rivers, especially highly turbid large rivers, have largely been ignored. The dataset used in this paper includes measured SSC and multi-temporal Landsat ETM+ images covering most part of the Yangtze River. Using an effective easy-to-use atmospheric correction method that does not require in situ atmospheric conditions, retrieved water reflectance of Band 4 was found to be a good SSC indicator within the large SSC range 22-2610 mg l(-1). The newly developed regression relation between SSC and water reflectance of Band 4 appears to be able to provide a relatively accurate SSC estimate directly from Landsat ETM+ images for the Yangtze River from the upper, the middle to the lower reaches. With the relation it is possible to estimate or map out SSC dynamics of large rivers which lack SSC data due to constraints of conventional measurements.
机译:悬浮泥沙浓度(SSC)是研究河流泥沙迁移和水质变化的关键参数,但是传统的测量方法既昂贵又费时。本文的重点是提出一种可能对估算SSC有用的方法,该方法对过程地貌和水文学至关重要。在以前的研究中,遥感技术已被用于估算单个Landsat卫星图像覆盖范围内可见的海水以及低浊度内陆水域(如湖泊,水库和短河段)的SSC。河流,特别是浑浊的大河流,在很大程度上被忽略了。本文使用的数据集包括测量的SSC和覆盖长江大部分地区的多时相Landsat ETM +图像。使用不需要现场大气条件的有效,易于使用的大气校正方法,发现波段4的回水反射率是在大SSC范围22-2610 mg l(-1)内的良好SSC指示剂。波段4的SSC和水反射率之间新建立的回归关系似乎能够直接从Landsat ETM +图像中的长江上游,中部到下游提供相对准确的SSC估计。利用该关系,可以估计或绘制出由于常规测量的限制而缺乏SSC数据的大河的SSC动态。

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