Assessment of suspended sediment mixing at the confluence of the Mississippi and Missouri rivers using broad-band satellite remote sensing

M. Umar, B. L. Rhoads, J. A. Greenberg

Research output: Chapter in Book/Report/Conference proceedingConference contribution

Abstract

Quantitative assessment of mixing of suspended sediment downstream of large river confluences poses enormous challenges because of the large scales involved. This paper presents a new approach to quantifying spatial patterns of mixing at and downstream of large river confluences based on satellite remote sensing. SSCs are modeled by calibrating a predictive model using spectral information from Landsat remote sensing with data on sediment loads collected at U.S. Geological Survey gaging stations. The model is used to predict the spatial distribution of SSCs over a 110 km reach of Mississippi River downstream from the confluence with the Missouri River. Mixing across and along the river is calculated at 500 m intervals based on spatial averaging of information with the intervals. An example of the results of the model are presented to illustrate its value in determining the factors that influence mixing downstream of confluences.

Original languageEnglish (US)
Title of host publicationRiver Flow - Proceedings of the International Conference on Fluvial Hydraulics, RIVER FLOW 2016
EditorsGeorge Constantinescu, Marcelo Garcia, Dan Hanes
PublisherCRC Press/Balkema
Pages1648-1654
Number of pages7
ISBN (Print)9781138029132
DOIs
StatePublished - 2016
EventInternational Conference on Fluvial Hydraulics, RIVER FLOW 2016 - St. Louis, United States
Duration: Jul 11 2016Jul 14 2016

Publication series

NameRiver Flow - Proceedings of the International Conference on Fluvial Hydraulics, RIVER FLOW 2016

Other

OtherInternational Conference on Fluvial Hydraulics, RIVER FLOW 2016
Country/TerritoryUnited States
CitySt. Louis
Period7/11/167/14/16

ASJC Scopus subject areas

  • Fluid Flow and Transfer Processes
  • Geotechnical Engineering and Engineering Geology

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