Remote-Sensing Method for Monitoring Suspended-Sediment Concentration on the Middle-Mississippi and Lower-Missouri Rivers

IF 0.9 Q4 WATER RESOURCES
Megan J. Martinez, Amanda L. Cox
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Abstract

Sediment transport, erosion, and deposition are primary drivers of river geomorphic processes and ecological services. Suspended-sediment concentration (SSC) is an important parameter for evaluating these processes and is accordingly of significant interest to engineers, scientists, and water resource managers. The United States Geological Survey (USGS) previously operated nine daily SSC gauging stations along the Mississippi River, with operating dates ranging from 1974 to 2018. Currently, there are no USGS gauging stations reporting daily SSC values along the Mississippi River. For this study, regression models were developed to compute the SSC along the Middle-Mississippi River (MMR) and Lower-Missouri River (LMOR) using publicly and freely available Landsat imagery. Surface reflectance data from Landsat satellites were used with USGS-measured SSC to develop regression models for three different Landsat sensors (Landsat 8 OLI/TIRS, Landsat 7 ETM+, and Landsat 4-5 TM). Previous models published for predicting SSC in the MMR and LMOR from Landsat images have a linear-regression form and have provided invalid negative values when extrapolated outside of the dataset used for development. The objectives of this study were to develop reflectance-SSC regression models using a power-function form and demonstrate their extrapolation performance using multiple novel applications in the MMR basin. The reflectance-SSC regression models were applied to the following conditions: 1) mixing at the Mississippi and Missouri River confluence, 2) point-source pollution, and 3) SSC changes along the entire MMR reach for a range of discharges. The regression models were also used to develop sediment rating curves for the four largest tributaries of the MMR.

Abstract Image

密西西比河中河和密苏里河下游悬浮泥沙浓度的遥感监测方法
输沙、侵蚀和沉积是河流地貌过程和生态服务的主要驱动力。悬浮泥沙浓度(SSC)是评估这些过程的一个重要参数,因此引起了工程师、科学家和水资源管理者的极大兴趣。美国地质调查局(USGS)此前在密西西比河沿岸运营9个每日SSC测量站,运营日期从1974年到2018年不等。目前,没有美国地质勘探局的测量站每天报告密西西比河沿岸的SSC值。在这项研究中,利用公开和免费的Landsat图像,开发了回归模型来计算密西西比河中游(MMR)和密苏里河下游(lor)的SSC。将Landsat卫星的地表反射率数据与美国地质调查局测量的SSC一起使用,为三种不同的Landsat传感器(Landsat 8 OLI/TIRS、Landsat 7 ETM+和Landsat 4‐5 TM)建立回归模型。以前发表的用于从Landsat图像预测MMR和lmors中的SSC的模型具有线性回归形式,并且在用于开发的数据集之外外推时提供了无效的负值。本研究的目的是利用幂函数形式建立反射率- SSC回归模型,并通过在MMR盆地的多种新应用证明其外推性能。反射率- SSC回归模型应用于以下条件:1)密西西比河和密苏里河汇合处的混合,2)点源污染,以及3)整个MMR河段的SSC变化。利用回归模型建立了MMR四大支流的泥沙等级曲线。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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